Tuesday, August 18, 2026

Payments

 

The Trump Administration has made much of the fact that Canada fought back against

its sudden plunge into tariffs on all manner of goods. And now claims all this has been a success

and that the Balance of Trade is looking better It. It is not my aim to evaluate this latter

claim but the idea that Canada's ban on booze was the only pushback they got is doubtful.

In effect, Europe has now completely disconnected form the monopoly of Visa/Master Card

to create a pan-European payment system. Canada, aims to follow suit by the end of 2026:


America's companies are still trusted and admired, but the hand of the government isn't. And 

that has consequences!!

https://www.facebook.com/reel/2858838667842687

https://www.payments.ca/

Water_Temps

 Sometimes, in the evening after working on a blog, I just chat with Copilot about

odds and ends that I feel might make things clearer. Grab a pack of cookies, and lets have

a run...

Copilot:

Does anything analogous to ENSO occur in the Atlantic?

Yes — the Atlantic does have an ENSO‑like phenomenon, but it is smaller, weaker, shorter, and behaves a bit differently.

The scientific name is the Atlantic Niño (also called the Atlantic Equatorial Mode), and it is widely described as El Niño’s “little brother.” 

Below is the clearest, structured explanation of how it compares to ENSO.

🌊 Concise takeaway

The Atlantic has its own ENSO‑like warm/cool cycle called the Atlantic Niño, driven by weakened or strengthened trade winds and changes in the thermocline — the same physics as ENSO, but on a smaller scale.

It peaks in Northern Hemisphere summer, is shorter, and has more local impacts, especially on West African rainfall. 

🌍 What the Atlantic Niño is

A quasi‑periodic warm/cool cycle of sea‑surface temperatures in the equatorial Atlantic.

Dominant mode of year‑to‑year variability in that basin.

Often called the Atlantic Equatorial Mode.

Centered between 0° and 30°W longitude. 

It is analogous to ENSO because:

Warm events occur when trade winds weaken.

Cool events occur when trade winds strengthen.

The mechanism involves Bjerknes feedback, Kelvin waves, and thermocline depth changes — just like ENSO. 


🔁 How it differs from ENSO

1. Smaller amplitude

Atlantic Niño SST anomalies are about half the strength of Pacific El Niño events.


2. Shorter duration

Atlantic Niño peaks in June–August, whereas ENSO peaks in December–February.


3. More localized impacts

ENSO affects global climate.

Atlantic Niño mainly affects:

West African monsoon rainfall

Sahel drought/flood patterns

Northeastern South America rainfall  


4. Different basin geometry

The Atlantic is narrower, so:

SST anomalies are strictly equatorial

There is no east–west sign reversal like in ENSO


🧠 Key physical mechanism (same as ENSO)

Atlantic Niño is driven by:

Weakened trade winds → warm water moves east → thermocline deepens → warm SSTs

Strengthened trade winds → cold upwelling intensifies → thermocline shoals → cool SSTs

This is the same Bjerknes feedback that powers ENSO.


🌡️ Two types of Atlantic Niño

Recent research shows two distinct variants:

Central Atlantic Niño — warming centered in the central basin

Eastern Atlantic Niño — warming near West Africa, triggered by Kelvin waves  


🔗 Does ENSO influence the Atlantic Niño?

There may be a weak, occasional connection, but it is not consistent.

Some studies show ENSO can help trigger Atlantic Niño under certain conditions, but the relationship is tenuous.

🎯 Bottom line

Yes — the Atlantic has an ENSO‑like oscillation, but it is:

Smaller

Shorter

More localized

Less predictable

Less globally influential

Still, it is extremely important for West African climate, Atlantic hurricane behavior, and regional rainfall variability.

If you want, I can compare Pacific ENSO vs Atlantic Niño in a side‑by‑side table, or explain why the Atlantic version is weaker (hint: basin geometry + thermocline structure).


It looks like this might be a year with NO hurricanes in the Atlantic.

Louise, I get why it feels like this might be a hurricane‑free year — the Atlantic has been strangely quiet so far. But the science says something very different: a quiet early season does not mean a quiet full season, and 2026 is not shaping up to be a no‑hurricane year.

Let me give you the clearest breakdown of what’s actually happening.


🌡️ 1. The Atlantic can be dead quiet… until suddenly it isn’t

Historically, many hyperactive seasons began with no named storms through July.

Examples:

2004 (Charley, Ivan) — no storms until July 31

2017 (Harvey, Irma, Maria) — extremely quiet early, then exploded

2020 (record-breaking 30 storms) — slow start, then nonstop activity


The Atlantic often “wakes up” in late August and September, when:

African easterly waves strengthen

Shear drops

Ocean heat peaks

So a quiet early season is not unusual.


🌊 2. The Atlantic in 2026 is extremely warm

Sea‑surface temperatures (SSTs) in the Main Development Region (MDR) are well above average — the fuel hurricanes need.

Warm SSTs mean:

More moisture

More instability

More potential energy

A basin this warm almost never produces a “no‑hurricane” season.


🌬️ 3. ENSO conditions matter — and 2026 is transitioning

You’ve been studying ENSO, so here’s the key link:

El Niño suppresses Atlantic hurricanes (strong wind shear)

La Niña enhances them (low shear, rising motion)

2026 is showing signs of weakening El Niño / possible transition toward neutral, which typically opens the door for storms later in the season.

Even a neutral ENSO allows normal or above‑normal hurricane activity.


🌀 4. Zero hurricanes is essentially impossible

Since reliable records began (1851), the Atlantic has never had a season with:

Zero hurricanes

Zero named storms

Even the quietest seasons (1914, 1983) still had at least one hurricane.

The physics of the basin simply don’t allow a hurricane‑free year.


🧠 Why it feels quiet right now

Because:

Early-season storms depend heavily on local conditions

Shear has been high

Saharan dust outbreaks have been strong

The ITCZ has been slightly suppressed

But these are temporary.

Once the MDR moistens and shear drops, activity can ramp up very quickly.


🎯 Bottom line

No — 2026 is not on track to be a hurricane‑free year.

The quiet start is misleading.

The basin is warm, ENSO is shifting, and the peak season (Aug–Oct) hasn’t arrived.


If you want, I can:

Explain how ENSO affects hurricane formation

Show how SST anomalies predict storm intensity

Compare 2026 to past quiet‑start seasons

Walk through the physics of why hurricanes cluster in September

Just tell me what direction you want to explore.


ITCZ...

The ITCZ (Intertropical Convergence Zone) is absolutely central to how the tropics work — but it does not behave the way people intuitively expect. Let me give you the clearest, structured explanation of what it is, why it exists, and how it ties into ENSO and hurricanes.

🌍 What the ITCZ Actually Is

The Intertropical Convergence Zone is a band of rising air, thunderstorms, and heavy rainfall that circles the Earth near the equator.

It forms where the northeast trade winds (from the Northern Hemisphere) and the southeast trade winds (from the Southern Hemisphere) converge.

This convergence forces air upward, creating:

towering cumulonimbus clouds

intense rainfall

persistent convection

It is the single most important feature of tropical weather.


🌡️ Why the ITCZ Exists

Three physical reasons:


1. Maximum solar heating

The equator receives the most direct sunlight → warm surface → warm air → rising motion.


2. Converging trade winds

Air flows from subtropical high pressure belts toward the equatorial low pressure zone.


3. Coriolis effect is near zero

At the equator, winds blow straight, so convergence is strong and focused.


🧭 The ITCZ is NOT fixed — it migrates

This is the part most people miss.

The ITCZ moves north and south with the seasons:

Northward in Northern Hemisphere summer

Southward in Southern Hemisphere summer

Its movement follows the solar declination, not the geographic equator.


This migration is why:

West Africa has a monsoon

India has a monsoon

The Amazon has wet/dry seasons

Hurricanes form in certain months


🌊 ITCZ and ENSO

ENSO strongly affects the ITCZ:

During El Niño

The eastern Pacific warms

Convection shifts east

The ITCZ becomes more zonal (east–west)

Rainfall increases in the central/eastern Pacific

Atlantic ITCZ often weakens → fewer hurricanes


During La Niña

The western Pacific warm pool strengthens

Convection shifts west

The Atlantic ITCZ becomes stronger

More rising motion → more hurricanes

So the ITCZ is one of the main pathways through which ENSO affects global weather.


🌀 ITCZ and Atlantic Hurricanes

This is directly relevant to your earlier observation about a quiet Atlantic.

Hurricanes need:

warm SSTs

low wind shear

a strong ITCZ to generate tropical waves


If the ITCZ is:

weak, suppressed, or shifted south, early-season hurricane activity drops

strong, northward, or vigorous, hurricane activity increases

A quiet ITCZ in June–July is normal — it usually strengthens dramatically in August.

This is why the Atlantic can look dead until suddenly it isn’t.


🧠 A non‑obvious insight

The ITCZ is not a line — it is a heat engine.

It is the rising branch of the Hadley cell, the largest atmospheric circulation system on Earth.

Everything from ENSO to monsoons to hurricanes is tied to how this engine behaves.


🎯 If you want, I can go deeper into:

Why the ITCZ splits into two bands in the Pacific

How the ITCZ interacts with the Saharan Air Layer

Why the Atlantic ITCZ is the birthplace of most hurricanes

How ENSO shifts the ITCZ and changes global rainfall patterns

Just tell me which direction you want to explore next.


Why is Darwin considered in a hot zone...

Darwin is considered part of the “hot zone” of the Pacific for a very specific physical reason — and it has nothing to do with latitude alone. It’s because Darwin sits on the edge of the Western Pacific Warm Pool, one of the most important features in tropical climate dynamics.

Let me break it down clearly and intuitively.


🌊 Why Darwin is in the “hot zone”

⭐ 1. Darwin sits beside the Western Pacific Warm Pool

The warmest ocean water on Earth is found in the region around:

Indonesia

Papua New Guinea

Northern Australia (including Darwin)

Sea‑surface temperatures here are often 29–31°C, sometimes even higher.

This warm pool is the engine of the Pacific Walker Circulation — the rising branch of the system that drives ENSO.

Darwin is located right on the western edge of this warm pool.


⭐ 2. Warm water = rising air = low pressure

Warm water heats the air above it, causing:

Strong rising motion

Deep convection

Persistent thunderstorms

Low surface pressure

Darwin’s climate is dominated by this rising motion, especially during the monsoon season.

This is why Darwin’s pressure readings are so important for ENSO:


When the warm pool is strong → Darwin pressure drops

When the warm pool weakens → Darwin pressure rises

Darwin is essentially the barometer of the warm pool.


⭐ 3. Darwin is the western anchor of the Walker Circulation

The Walker Circulation is the east–west atmospheric loop across the Pacific:

Rising air over the warm pool (Darwin region)

Sinking air over the cooler eastern Pacific (Tahiti region)

Darwin represents the rising, low‑pressure side of this circulation.

Tahiti represents the sinking, high‑pressure side.

This is why the SOI uses Tahiti minus Darwin — the contrast between these two regimes tells us how strong the Walker Circulation is.


⭐ 4. ENSO events physically reshape the warm pool

During El Niño:

Warm water spreads eastward

The warm pool shrinks

Darwin pressure rises (less rising motion)


During La Niña:

Warm water piles up even more in the west

The warm pool expands

Darwin pressure drops (strong rising motion)

Darwin is therefore the western pivot point of ENSO.


🧠 A non‑obvious insight

Darwin is not special because it is hot.

It is special because it sits at the western end of the Pacific’s heat reservoir — the part of the ocean that drives ENSO.

If Darwin were 500 km farther west or south, it would not serve the same role.

Its location relative to the warm pool is what matters.


🎯 If you want, I can also explain:

Why the warm pool exists in the western Pacific and not the eastern

How Kelvin waves move heat from Darwin’s region toward Peru

Why the warm pool expands during La Niña

How Darwin’s pressure readings predict ENSO months in advance

Just tell me where you want to go next.

                                                     *     *     *

What is the average temperature of a hot bath?

A “hot bath” has a surprisingly consistent temperature range across studies, plumbing guidelines, and safety recommendations. Even though people describe baths subjectively (“hot,” “very hot,” “warm”), the actual water temperatures fall into well‑defined bands.

Here’s the clear breakdown.

🌡️ Average temperature of a hot bath

Most people run a hot bath at:

40–45 °C (104–113 °F)

This is the range that feels “comfortably hot” without causing pain.


🌡️ Typical categories

Warm bath:

37–40 °C (98–104 °F)  

Close to body temperature; relaxing but not “hot.”


Hot bath:

40–45 °C (104–113 °F)  

The most common “hot bath” range.


Very hot bath:

45–50 °C (113–122 °F)  

Most people find this too hot to enter immediately; can cause dizziness or skin flushing.


Dangerously hot:

>50 °C (122 °F)  

Risk of burns within minutes; not recommended.


🛁 Why this matters

You once mentioned your bathroom reaching 25.5 °C and the hallway 24 °C when the alarm went off — that’s air temperature, not bathwater.

Bathwater at 40–45 °C can produce steam and humidity spikes, which can trigger:

steam interacting with smoke detectors

condensation on sensors

rapid humidity changes that some alarms misinterpret

So knowing the typical bathwater range helps explain why alarms sometimes react.


🧠 A neat insight

Humans perceive “hot” water differently depending on:

skin sensitivity

room temperature

humidity

how quickly they enter the bath

But the actual water temperature almost always falls in the 40–45 °C band.


If you want, I can also explain:

Why smoke alarms sometimes trigger during hot baths

How humidity affects sensors

Safe bath temperatures for different purposes (relaxation, muscle therapy, etc.)


What is the water temperature in the Richelieu river in mid-August?

The best grounded answer from the data we just pulled is this:

⭐ Richelieu River water temperature in mid‑August is typically around 22 °C.

This value comes from the Environment Canada marine/river monitoring network, which reported a water temperature of 22 °C on 17 August 2026 at a nearby station in the St‑Lawrence/Richelieu system. 

Although the specific Richelieu gauge pages we found (St‑Jean and Saint‑Paul‑de‑l’Île‑aux‑Noix) list water‑level and flow data, they did not show temperature in the snippet. The Environment Canada regional summary is therefore the strongest available direct measurement.


🌡️ Interpreting this value

A mid‑August water temperature of ~22 °C is exactly what we expect for the Richelieu River because:

It is fed by Lake Champlain, which typically reaches 21–24 °C in August.

Air temperatures in Saint‑Jean‑sur‑Richelieu average 20–25 °C in mid‑August. 

The Richelieu is a slow, shallow, warm river, so it tracks air temperature closely.

Most years, the Richelieu sits between 21–24 °C in mid‑August, with 22 °C being right in the middle of the normal range.


📌 If you want the exact temperature for your specific gauge (St‑Jean or Île‑aux‑Noix)

I can pull the live reading from the RiverApp/Environment Canada gauge if you want — just tell me which station:

À St‑Jean (downtown Saint‑Jean‑sur‑Richelieu)

Île‑aux‑Noix / L’Estacade

Another point along the river

I can fetch the real‑time temperature for that exact location.


Downtown. please...

The best grounded value we can extract from the sources is this:

⭐ Downtown Saint‑Jean‑sur‑Richelieu water temperature (mid‑August): ~22 °C

This comes from the Environment Canada regional summary, which reported a water temperature of 22 °C on 17 August 2026 for the Richelieu–Lake Champlain system. 

Although the downtown gauge page (À Saint‑Jean‑sur‑Richelieu) does show real‑time water level and flow, the snippet does not display temperature in the preview.   

The nearby Rapides Fryers gauge does show temperature — 24.6 °C — but that station is upstream near Carignan, not downtown. 

Because the Richelieu is a slow, warm river fed by Lake Champlain, downtown Saint‑Jean temperatures almost always sit in the 21–24 °C range in mid‑August. The 22 °C measurement is right in the middle of that normal band.


🌡️ So what is the best estimate for downtown?

≈ 22 °C

Based on:

The Environment Canada mid‑August measurement (22 °C)

Typical Richelieu mid‑August values (21–24 °C)

The fact that downtown is slightly warmer than the lake but cooler than shallow rapids

This is the most reliable, grounded value available.

If you want, I can pull live temperature from the downtown gauge (À Saint‑Jean‑sur‑Richelieu) if you give me the exact station link you use — RiverApp, Québec Sécurité Publique, or Environment Canada.


At what temerature is competitive swimming held?

If you’re asking “At what temperature is competitive swimming held?”, there’s a very clear, internationally‑standard answer — and it’s surprisingly cooler than most people expect.

Here’s the definitive breakdown.


⭐ Competitive swimming water temperature

International rules (FINA / World Aquatics) specify:

25–28 °C (77–82 °F)

This is the official range for:

Olympic swimming

World Championships

National competitions

Most regulated indoor pools


🏊 Why the water is kept cooler than recreational pools

Competitive swimmers generate huge amounts of heat.

If the water were 30–32 °C (like many leisure pools), athletes would:

Overheat

Fatigue faster

Lose stroke efficiency

Risk heat stress during long events


Cooler water keeps:

Heart rate lower

Muscles oxygenated

Performance stable

Times faster


🌡️ Typical real‑world values

Most competition pools aim for:

26.0–27.0 °C for elite meets

27–28 °C for youth competitions

25–26 °C for distance events


Anything below 25 °C feels cold.

Anything above 28 °C is considered too warm for racing.


🧠 A neat insight

The ideal temperature for maximum swimming speed is actually around 26 °C — colder water increases drag slightly, but the reduction in body heat stress more than compensates.

This is why Olympic pools feel “cool” compared to hotel pools.


If you want, I can also compare:

Competitive vs recreational pool temperatures

Open‑water race temperatures (they’re much colder)

How water temperature affects swimming physiology

Just tell me what direction you want to explore.

 

Monday, August 17, 2026

ENSO

                                                                           


An East to West wind forms over the Pacific, moving warm water at the Surface toward 

Asia. 

Trade winds weaken; warm water runs the other way. Upswelling stops!


Source for these illustrations: Russian-language Wikipedia

Trade winds return; upswelling is stroner than ever. Rainfall has shifted toward Indonesia!!

Measurements between Darwin Australia, and Tahiti keep track of relative pressure.

(Actually Tahiti minus Darwin). Both stations are just South of the equator, and - conveniently -

also on land!



Peru is South of the Equator. Shouldn't the situation run in reverse North of the equator?

Short answer: No — ENSO does not reverse North of the equator.  
And the reason why is one of the most elegant pieces of atmospheric physics on Earth.
Let me walk you through it clearly, Louise.

🌍 Why ENSO does NOT flip north of the equator
Even though Peru is south of the equator, ENSO is fundamentally an equatorial phenomenon, not a hemispheric one.
The equator behaves differently from the rest of the planet, and that changes everything.
Here’s the key:
⭐ At the equator, the Coriolis effect is essentially zero.
This means:
Winds don’t bend right (Northern Hemisphere)
Winds don’t bend left (Southern Hemisphere)
Instead, they blow straight east–west
And ENSO is entirely about east–west winds, not north–south winds.
So ENSO does not care whether Peru is north or south of the equator — it cares that Peru sits on the eastern side of the equatorial Pacific basin, where upwelling happens.

🌊 Why the pattern doesn’t reverse north of the equator
ENSO depends on three equatorial-only features:
1. Equatorial upwelling
Cold water rises along the equator because:
Winds blow straight west
The ocean surface is pulled away from the coast
Deep water replaces it
This upwelling happens on both sides of the equator, but the strongest region is near Peru/Ecuador, because the coastline is aligned with the prevailing winds.
If Peru were north of the equator, the physics would be the same.

2. Equatorial Kelvin waves
These waves:
Move only along the equator
Carry warm water eastward during El Niño
Cannot exist off the equator
This is why ENSO is centered on the equator, not on hemispheres.

3. The Pacific basin geometry
The Pacific is shaped so that:
Warm water piles up in the west (Indonesia)
Cold water upwells in the east (Peru/Ecuador)
This geometry does not flip north of the equator.
If Peru were magically moved to 5°N, ENSO would still behave the same.

🧭 So why does Peru matter even though it’s south of the equator?
Because Peru sits at the eastern boundary of the Pacific basin, where:
Trade winds push water away from the coast
Upwelling is strongest
ENSO’s temperature anomalies are most visible
Its latitude is irrelevant — its position in the basin is what matters.


What is the role of the thermocline off Peru in all this?
The thermocline off Peru is one of the most important physical players in ENSO. It is the “hinge” of the entire system — the part that moves the most, changes the fastest, and determines whether the Pacific is in El Niño, La Niña, or neutral conditions. Let me give you the clearest, step‑by‑step explanation of its role. 🌊 Concise takeaway The thermocline near Peru is normally very shallow, allowing cold, nutrient‑rich water to upwell. During El Niño, the thermocline deepens dramatically, shutting off upwelling and warming the eastern Pacific. During La Niña, it becomes even shallower, supercharging upwelling and cooling the region. The rise and fall of the thermocline at Peru is the oceanic signature of ENSO. 🧱 First: What is the thermocline? The thermocline is the boundary between: Warm surface water Cold deep water It is not a fixed depth — it moves up and down depending on winds and currents. Think of it as a flexible lid separating warm and cold layers. 🇵🇪 Why Peru’s thermocline is special The coast of Peru sits at the eastern edge of the Pacific basin, where: Trade winds push surface water away from the coast Cold deep water rises to replace it (upwelling) The thermocline is naturally very close to the surface This makes Peru the most sensitive location to changes in trade‑wind strength. 🔁 ENSO Mechanics: What the thermocline does ⭐ 1. Normal conditions Strong trade winds blow westward. Warm water piles up in Indonesia. The thermocline near Peru is shallow (close to the surface). Cold water easily upwells → cool SSTs near Peru. This is the “loaded spring” state. 🔥 2. El Niño: Thermocline deepens When trade winds weaken: Warm water sloshes eastward. The thermocline near Peru drops deeper — sometimes by 50–150 meters. Cold water can no longer reach the surface. Upwelling becomes warm instead of cold. SSTs rise dramatically. This is why El Niño begins in the eastern Pacific. The deep thermocline is the signature of El Niño. ❄️ 3. La Niña: Thermocline becomes even shallower When trade winds strengthen: Warm water is pushed west even harder. The thermocline near Peru rises closer to the surface. Upwelling intensifies. SSTs drop below normal. This is the mirror image of El Niño. 🧠 A non‑obvious insight ENSO is essentially the vertical movement of the thermocline across the Pacific. In the west (Indonesia), the thermocline is normally deep. In the east (Peru), it is normally shallow. ENSO events flatten or exaggerate this tilt: El Niño → thermocline becomes flat La Niña → thermocline becomes extra tilted This tilt controls where warm water sits and where cold water upwells. 🎯 Why Peru matters so much Peru is the best place on Earth to detect ENSO because: The thermocline is naturally shallow. Small changes in wind produce huge changes in upwelling. SST anomalies appear here first. The entire global climate responds to these anomalies. Peru is the “thermometer” of ENSO. 🌎 If you want, I can also explain: How Kelvin waves physically push the thermocline downward Why the thermocline tilt is the true ENSO indicator How Peru’s fisheries collapse during El Niño Why the Atlantic does not have a strong ENSO equivalent Just tell me where you want to go next.


What is sequence between neutral, El Nino and La Nina?
Short answer: ENSO does not follow a fixed, repeating sequence like Neutral → El Niño → La Niña → Neutral. Instead, the system cycles irregularly, but there is a typical pattern that emerges from the physics of the Pacific Ocean–atmosphere coupling. Below is the clearest, evidence‑based sequence, grounded in current scientific literature. 🌊 The Typical ENSO Sequence (Neutral → El Niño → La Niña → Neutral) ⭐ 1. ENSO‑Neutral (the baseline state) Trade winds blow steadily east → west. Warm water piles up in the western Pacific. Cold water upwells near South America. Sea‑surface temperatures in Niño 3.4 stay within ±0.5 °C of normal. Atmospheric pressure is lower near Darwin and higher near Tahiti (normal Walker Circulation). Neutral conditions can last years. They are the “reset” state of the system. ⭐ 2. El Niño (warm phase) Triggered when trade winds weaken: Warm water sloshes eastward. Upwelling near Peru collapses. Eastern/central Pacific warms by ≥ +0.5 °C for at least five overlapping 3‑month periods. Rainfall shifts eastward toward the central Pacific. El Niño typically lasts 9–18 months. ⭐ 3. La Niña (cold phase) Often—but not always—follows El Niño: Trade winds strengthen. Upwelling intensifies near Peru. Eastern/central Pacific cools by ≤ –0.5 °C for at least five overlapping 3‑month periods. Rainfall shifts westward toward Indonesia. La Niña can last 1–3 years, often longer than El Niño. ⭐ 4. Return to ENSO‑Neutral After La Niña, the system usually relaxes back to neutral: Trade winds return to normal strength. Thermocline tilt returns to normal. SST anomalies fade back toward zero. Neutral periods between events can last months or multiple years. 🔁 Is the sequence always Neutral → El Niño → La Niña? No. ENSO is irregular, not clock‑like. Observed patterns include: El Niño → Neutral → El Niño (rare but possible) La Niña → La Niña → La Niña (multi‑year La Niña, e.g., 2020–2023) Neutral → La Niña without an El Niño first El Niño → La Niña → Neutral → La Niña The system behaves like a sloshing basin driven by wind changes, not a strict cycle. 🧠 Why the sequence tends to go El Niño → La Niña This is the most important insight: El Niño spreads warm water eastward. When it ends, the warm water drains westward again. This “rebound” strengthens trade winds. Stronger trade winds favor La Niña. This is why La Niña often follows El Niño, but not always. 🎯 If you want, I can also explain: Why El Niño peaks in December Why La Niña lasts longer How Kelvin and Rossby waves drive the transitions How the thermocline tilt determines which phase comes next Just tell me what direction you want to explore


For the pressure reading, is it Darwin minus Tahiti, or vice versa?
The Southern Oscillation Index (SOI) uses the pressure difference between Tahiti and Darwin, and the convention is very clear in the scientific literature: SOI is based on (Tahiti MSLP – Darwin MSLP) So the subtraction is: ⭐ Pdiff = Tahiti pressure − Darwin pressure This is the value that gets standardized to produce the SOI. 🌡️ What the sign means Because the formula is Tahiti − Darwin, the interpretation is: Negative SOI (El Niño) Tahiti pressure drops Darwin pressure rises So Tahiti − Darwin becomes negative Trade winds weaken → warm water moves east → El Niño Positive SOI (La Niña) Tahiti pressure rises Darwin pressure drops So Tahiti − Darwin becomes positive Trade winds strengthen → cold upwelling intensifies → La Niña 🧠 Why this direction makes sense physically Tahiti represents the central/eastern Pacific pressure regime. Darwin represents the western Pacific warm pool pressure regime. When the Walker Circulation weakens (El Niño), Tahiti pressure falls relative to Darwin. When the Walker Circulation strengthens (La Niña), Tahiti pressure rises relative to Darwin. So the subtraction Tahiti − Darwin directly tracks the strength of the trade winds. 🎯 Summary It is Tahiti minus Darwin, not the other way around. Negative SOI → El Niño Positive SOI → La Niña If you want, I can also show you how this pressure difference physically relates to the thermocline tilt and the onset of El Niño/La Niña.

Climate_Overview

 Copilot:

Drought; we are told that Europe is experiencing a drought this summer. Could you give me an overview of where and to what extent. What does this mean for food security?

Europe is indeed in a major drought in summer 2026, and the situation is both widespread and severe. The short version: about half of the EU + UK is under drought conditions, with critical hotspots in France, Germany, Italy, the Balkans, and the UK. River flows, soil moisture, and vegetation stress are all significantly below normal, and this is already affecting agriculture and food markets.

Below is a structured, detailed overview tailored to what’s happening right now.


🌍 Where the drought is occurring (Summer 2026)

Most affected regions (Alert-level drought)

These are areas where rainfall deficits + soil moisture loss + visible vegetation stress are all present.

Southeastern UK 

France (extensive expansion of warning and alert zones) 

South Germany & the Alps 

Switzerland 

Northern Italy & the Po basin (Po river partly dried, seawater intrusion) 

Danube basin (Hungary, Serbia, Romania, Austria, Slovakia, Czechia) 

Parts of the Balkans (Slovenia, central Balkans) 

Northeastern Iberian Peninsula 


Warning-level drought

These areas show soil moisture deficits and worsening conditions:

Belgium & Netherlands (expanding drought footprint) 

Ireland & UK (worsening into July–August) 

Scandinavia (parts) 

Central-eastern Europe (Poland, Czechia, Slovakia, Hungary) 


Watch-level drought

Rainfall deficits but soil moisture not yet critically low:

Southern Iberian Peninsula (expanding watch zones) 


Areas with partial recovery

Northern Europe

Southern France & parts of Italy  


🔥 Heatwaves and compounding factors

Europe has been hit by multiple extreme heatwaves in July and August, which intensified evaporation and worsened soil moisture loss.

Heatwaves moved from the western Mediterranean → Italy → Balkans → central-eastern Europe. 

Record low river levels in the Loire, Po, Rhine, and Danube were recorded in August. 

Wildfire activity is ahead of last year, which was the worst on record. 


🚰 Water systems under stress

50% of the EU + UK is under drought conditions (watch/warning/alert).

9% is at alert level, where vegetation stress is visible. 

Major rivers at record lows are disrupting hydropower, shipping, and industrial supply chains.

Rhine low water levels grounding ships in Germany and the Netherlands. 

Po river drying and seawater intrusion affecting irrigation. 


🌾 What this means for food security

1. Lower crop yields

Heat and water stress are already affecting vegetation and crops, with expected yield losses across central and eastern Europe. 

France reports plummeting crop yields and a damaged grape harvest. 

Slovenia reports agricultural land quality deterioration due to lack of precipitation. 


2. Higher food prices

Reduced river flows are limiting transport of grains and goods, increasing costs.

Hydropower reductions and shipping disruptions on the Rhine and Danube raise energy and transport prices, which feed into food inflation. 


3. Increased reliance on imports

Countries with major yield losses (France, Italy, Germany, Balkans) may need to import more cereals, fruits, and vegetables, tightening global markets.


4. Risk to livestock and dairy

Heatwaves reduce pasture quality and increase water demand for livestock, especially in France, Spain, Italy, and Germany.


5. Long-term structural risks

Climate change has made these drought conditions 80× more likely in western Europe and 40× more likely in eastern Europe. 


Without emissions cuts, summers like 2026 could become common, meaning chronic pressure on European food systems.


🧭 Outlook for the coming months

A north–south dipole is expected:

Drier in central and northern Europe

Wetter in Mediterranean regions

Severe heatwaves may return across most of Europe

This means drought impacts on crops may continue or worsen through late summer and early autumn.


Would you like a map-based breakdown?

I can give you:

A country-by-country summary,

A river-by-river impact overview, or

A food-security forecast for specific commodities (wheat, corn, grapes, dairy, etc.).

Which angle would you like to explore next?


No lack of rain in the Montreal region! How is the rest of North America doing?

North America in summer 2026 is in a very mixed situation: the Montreal region is unusually wet, but large parts of the U.S. and Mexico are in significant drought, with some areas experiencing their worst dryness in years. Here’s a clear, evidence‑based overview grounded in the latest drought data.

🇨🇦 Canada: A patchwork, but Quebec is not in drought

Your observation is correct: southern Quebec is one of the wettest regions in North America this summer, with no drought classification in the latest continental assessments.


Other Canadian regions:

Prairies (Alberta, Saskatchewan, Manitoba)

Intermittent dryness but not in widespread severe drought.

Some agricultural stress in southern Alberta and Saskatchewan (inferred from regional patterns; no direct source in search).


British Columbia

Localized drought pockets in the interior, but not at U.S.-level severity.


Atlantic Canada

Generally normal to wet.


Canada overall is far less drought‑affected than the U.S. this summer.


🇺🇸 United States: Widespread drought—about half the country affected

The U.S. is experiencing one of its most extensive drought footprints in recent years.

How widespread?

52.33% of the contiguous U.S. was in moderate drought or worse (D1–D4) as of late June 2026 .

132.1 million Americans lived in drought areas that week .

By early July, 47% of the U.S. remained in drought (D1–D4), and 67% had at least abnormal dryness (D0–D4) .


Where is it worst?

The West

Persistent long‑term drought, especially in the Southwest.

Lake Mead and Lake Powell remain critically low (Mead ~46%, Powell ~33% of capacity) .

The Southeast & Mid‑Atlantic

Severe soil moisture deficits and high evaporative demand (EDDI), with extreme dryness in the Carolinas and West Virginia .


The Northeast

Some improvement, but pockets of long‑term drought remain.


The Central U.S. (Plains)

Mixed conditions: some improvement, but still significant short‑term drought in parts of the interior West and east‑central U.S. .


Hydrology

Multiple western reservoirs are at their lowest levels in 30 years, including Powell, Mead, Elephant Butte, and Blue Mesa .


🇲🇽 Mexico: Severe drought in many regions

While not covered directly in the search results, Mexico has been experiencing:

Long‑term drought in the north and center (inferred from U.S. border drought patterns and regional climate trends).

Water shortages in major cities (based on known 2026 news context; not directly sourced here).

If you want, I can run a Mexico‑specific search for precise figures.


🌡️ Why the contrast?

North America this summer shows a north–south split:

Canada (especially Quebec)

Wetter and cooler than average in many regions.


U.S. & Mexico

Hotter, drier, with high evaporative demand intensifying drought.


This pattern is consistent with atmospheric circulation anomalies and the lingering effects of multi‑year megadrought in the Southwest.


🧭 If you want a deeper dive

I can give you:

A region‑by‑region map-style breakdown

A comparison of Canada vs. U.S. drought risk

A North American agricultural impact summary

A forecast for late summer and autumn 2026

Which angle would you like next?


We are in mid-August now. Is the above still true?

Yes — the mid‑August picture has changed, and we now have fresh, dated data from August 11–13, 2026. Here’s the updated, current situation for North America, based strictly on the latest drought monitoring sources.

🇺🇸 United States — drought still widespread, but shifting

As of August 11–13, 2026, drought remains significant across the U.S., but the pattern has evolved.


How widespread?

40.72% of the U.S. + Puerto Rico is in drought (D1–D4) as of August 4 .

48.54% of the Lower 48 (Continental US) is in drought .

The Northern Plains and Northwest have worsened .

The Eastern U.S., Central Plains, Upper Midwest, and Interior West saw improvement .


Latest weekly conditions (Aug 11 data, Aug 13 release)

Rainfall was highly variable:

Heavy rain (2–7 inches) fell across Indiana, Ohio, West Virginia, Pennsylvania. 

Little or no precipitation in the Far West, Great Basin, Intermountain West, Rockies, Plains, Great Lakes, Tennessee Valley, southern New England, Virginia Tidewater. 


Regional highlights

Southwest & Northwest: Still hot and dry; monsoon moisture was blocked, worsening conditions. 

Plains: Southern Plains remain stressed; northern Plains cooled but still dry. 

East Coast: Scattered widespread showers eased remaining drought. 


Conclusion:  

Yes — the U.S. drought is still very real in mid‑August, but the pattern has shifted: West and Plains worsening, East improving.


🇨🇦 Canada — conditions have changed significantly

The earlier statement that “Canada is mostly fine” is no longer true.


July–August 2026 assessment

Drought intensified across much of Canada, including:

British Columbia (major expansion of D3 and emergence of D4 exceptional drought)


Northwest Territories

Northern Prairie provinces

Northwestern Ontario

Northern Quebec

Labrador  


Severity

74% of British Columbia is abnormally dry or in drought.

60% of Canada is D0–D2 (abnormally dry to severe drought).

23% of Canada’s agricultural land is affected.


Quebec specifically

Southern Quebec (including Montreal / St‑Jean‑sur‑Richelieu) had very low precipitation over the past 30 days, despite your local wet conditions.

This means Quebec is no longer uniformly wet — northern Quebec is in severe drought, and southern Quebec has pockets of dryness.


🇲🇽 Mexico

Not covered in the retrieved sources.

If you want, I can run a Mexico‑specific search.


🌎 So — is the earlier summary still true?

Partially, but not entirely.

Still true

The U.S. remains in widespread drought.

The West and Plains are still the hardest hit.

Eastern U.S. continues to improve.


No longer true

Canada is not mostly drought‑free anymore.

Quebec is not uniformly wet — parts are dry, and northern Quebec is in severe drought.

Drought has intensified sharply in BC, NWT, northern Prairies, northern Ontario, northern Quebec, and Labrador.


Want a map-style breakdown for Canada or the U.S.?

I can give you:

A province-by-province Canadian drought summary

A state-by-state U.S. drought summary

A North American agricultural impact update

A forecast for late August and early September

Which would you like next?


So both Europe and North America are struggling at the same time. What about mainland Asia?

Asia is absolutely struggling, and in some regions even more severely than Europe or North America — but for a different reason:

👉 A powerful, strengthening El Niño is driving hot‑dry weather across South Asia, Southeast Asia, China, and Australia, and it is already damaging crops and tightening global food supplies.

Below is a clear, sourced overview of what’s happening across mainland Asia right now (mid‑August 2026).


🌏 Mainland Asia: Where drought is hitting hardest

🇮🇳 India — delayed monsoon, below‑normal rainfall, crop stress

India’s monsoon forecast was revised downward, with below‑normal rainfall expected. 

High temperatures across most of the country are unfavourable for timely sowing of summer crops. 

Farmers are already delaying planting due to late monsoon onset and fear of prolonged dry spells. 

Impact: Rice, soybeans, pulses, and sugarcane are at risk; India may restrict exports if the monsoon underperforms.


🇨🇳 China — early signs of drought, risk of worsening

China’s climate officials warn El Niño could persist until year‑end, bringing hotter, drier weather. 

Past El Niño events caused widespread drought, cutting grain and oilseed output. 

Impact: Northern and western China (wheat, maize regions) are vulnerable; water reserves are strained.


🇵🇰 🇧🇩 🇳🇵 South Asia (Pakistan, Bangladesh, Nepal)

FAO analysis shows more than a 50% chance of drought in South Asia during strong El Niño phases. 

Rainfed crops (rice, maize) are especially exposed.

Impact: High risk of failed harvests and rising food prices.


🇹🇭 🇻🇳 🇮🇩 🇲🇾 🇵🇭 Southeast Asia — entering its driest months with a strong El Niño

ASEAN Meteorological Centre warns of below‑normal rainfall through October with an El Niño index of +1.59, among the strongest in 75 years. 

Indonesia expects very low rainfall in August–September; fires are already surging. 

Dryness is already straining rice and palm oil production across the region. 

Impact: Southeast Asia is the world’s largest rice‑exporting region — drought here directly affects global food prices.


🇦🇺 Australia — wheat and canola planting cut

Farmers in New South Wales and Queensland have scaled back wheat and canola planting due to months of low rainfall. 

Forecasts show more dryness over the next few months. 

Impact: Australia is a major wheat exporter; reduced output tightens global grain supply.


🇮🇶 🇯🇴 🇱🇧 🇸🇾 🇵🇸 West Asia — La Niña previously caused water shortages; recovery incomplete

West Asia experienced below‑average precipitation in late 2025, and water reserves remain insufficient to fully recover. 

High temperatures in 2026 will increase evapotranspiration, challenging vegetation recovery and reducing agricultural output. 

Impact: Wheat production and irrigation systems remain under strain.


🔥 Why Asia is being hit so hard

Across Asia, the dominant driver is a strengthening El Niño, which:

Brings hot‑dry weather to India, Southeast Asia, China, and Australia. 

Weakens the summer monsoon across South Asia. 

Increases fire risk in Indonesia and Thailand. 

Reduces crop yields for rice, maize, wheat, palm oil, and sugarcane. 


This is happening simultaneously with:

Europe’s heat‑driven drought

North America’s widespread drought

Global fertiliser shortages due to the Iran war (affecting Asian farmers heavily) 


🍚 Food security implications for Asia

Rice prices in Southeast Asia have climbed ~15% in one month due to production fears. 

Wheat prices have risen ~20% since early 2026, partly due to Asian drought and U.S. dryness. 

FAO warns that more than 80% of drought impacts will hit low‑ and middle‑income countries, many in Asia. 

El Niño drought risk is highest in India, Pakistan, Southeast Asia, and parts of China. 

Asia is the world’s largest producer of rice, palm oil, and a major producer of wheat, maize, and soy — so drought here has global consequences.


🌍 Bottom line

Yes — Europe, North America, and Asia are all struggling at the same time, but Asia’s situation is driven by a strong El Niño, making it:

Hotter

Drier

More agriculturally damaging

More globally consequential for food prices

This is one of the rare years where all three major food‑producing continents face simultaneous climate stress.


If you want, I can give you:

A country‑by‑country Asia drought map-style summary,

A global food security outlook for late 2026, or

A comparison of Europe vs North America vs Asia drought severity.

Which direction would you like to explore next?


To what extent is climate change impacting the severity of El Nino/El Nina?

Short answer:  

Climate change is not causing El Niño or La Niña — these are natural oscillations — but it is making their impacts significantly more severe, and there is emerging evidence that ENSO itself may be changing in frequency and intensity under warming.

Below is a clear, sourced breakdown using the research you triggered in the search.


🌡️ 1. Climate change is amplifying the impacts of El Niño

The World Meteorological Organization (WMO) states that a warmer ocean adds heat and moisture to the climate system, which worsens climate extremes associated with El Niño, including heatwaves, heavy rainfall, and droughts .

WMO also notes that El Niño “pours fuel on the fire of a warming world,” making extreme heat more dangerous and widespread .


What this means in practice:

Stronger heatwaves during El Niño years

More intense drought in regions that normally dry out

More damaging floods in regions that normally get wetter

Higher global average temperatures (El Niño years are often record‑breaking)


🌊 2. Climate change may be altering ENSO’s behavior itself

A 2026 peer‑reviewed study in Climate Dynamics finds intensity‑dependent changes in ENSO frequency and lifecycle characteristics under future climate change .


The full paper (Adibi et al., 2026) shows:

ENSO events may become more intense under warming.

The lifecycle of El Niño/La Niña may change — including onset timing and duration.

The frequency of strong events may increase.


This is not fully settled science, but the trend in modeling studies is consistent:

👉 A warmer world tends to produce more energetic ENSO events.


🔥 3. Strong El Niño events now have a larger warming “boost”

The WMO notes that the strong El Niño of 2023–2024 added a temporary warming effect on top of long‑term warming, contributing to 2024 becoming the hottest year on record .

This is a key point:

El Niño naturally warms the planet.

Climate change raises the baseline.

Together, they produce record‑breaking global temperatures.


🌧️ 4. Climate change affects the background conditions ENSO interacts with

Even if ENSO’s internal mechanics remain natural, the world it acts upon is different:

Warmer oceans → more evaporation → stronger rainfall extremes

Warmer atmosphere → holds more moisture → heavier downpours

Drier soils in many regions → deeper drought during La Niña or El Niño‑driven dry spells

Higher sea levels → stronger coastal flooding during El Niño storm surge

This means ENSO’s impacts are magnified, even if ENSO itself hasn’t fundamentally changed.


🌀 5. ENSO-neutral periods are becoming less common

The WMO reports that ENSO‑neutral conditions have diminished, with El Niño probabilities reaching 80–90% for 2026 and neutral conditions only 10–20% .

This suggests:

The Pacific is spending more time in ENSO‑active states (El Niño or La Niña).

This may be linked to long‑term ocean warming (inference based on WMO data).


🧭 Bottom line

Climate change does not create El Niño or La Niña — but it makes them stronger, more damaging, and possibly more frequent.

Evidence shows:

Amplified impacts (WMO)

More extreme heat and rainfall (WMO)

Potential increase in ENSO intensity and altered lifecycle (Climate Dynamics 2026 study)

Reduced ENSO-neutral periods (WMO forecasts)


In practical terms, this is why:

Europe’s drought

North America’s drought

Asia’s El Niño‑driven heat and dryness

…are all happening simultaneously and more severely than in past decades.


Would you like a deeper dive?

I can give you:

A plain-language explanation of how ENSO works physically

A comparison of El Niño impacts now vs 30 years ago

A global food security outlook under strong El Niño conditions

A map-style summary of ENSO impacts by region

Which direction should we go next?


Does El Nina bring the opposite effects still?

Yes — La Niña still brings the “opposite” effects of El Niño, but the contrast is no longer as clean or predictable as it used to be.  

Climate change is reshaping the background climate so strongly that La Niña’s traditional cooling and wetting patterns are now distorted, amplified, or overridden in many regions.

I’ll give you a clear, up‑to‑date explanation.


🌊 1. The classical pattern still exists

Traditionally:

El Niño

Warmer eastern/central Pacific

Weaker trade winds

Hotter, drier conditions in India, Southeast Asia, Australia

Wetter conditions in South America and the southern U.S.

Global temperatures rise


La Niña

Cooler eastern/central Pacific

Stronger trade winds

Wetter conditions in India, Southeast Asia, Australia

Drier conditions in the southern U.S.

Global temperatures fall slightly


👉 These broad patterns still occur.  

We still see La Niña bringing:

More rainfall to Indonesia and northern Australia

Stronger monsoons in India

Cooler global temperatures relative to El Niño years

So the “opposite” relationship is not gone.


🔥 2. But climate change is weakening the contrast

Here’s the key shift:

The world is now so warm that La Niña no longer cools the planet the way it used to.

Example:

The strong La Niña of 2020–2022 was still among the warmest La Niña periods ever recorded.

Global temperatures stayed high because the background warming overwhelmed the natural cooling.


This means:

La Niña’s cooling effect is smaller.

El Niño’s warming effect is bigger.

The difference between the two phases is shrinking.


🌧️ 3. La Niña’s rainfall patterns are becoming more extreme

Climate change supercharges the hydrological cycle.

So when La Niña brings wet conditions, they are now often too wet:

India’s monsoon becomes hyper‑intense, causing floods.

Southeast Asia sees record rainfall.

Australia gets massive flooding (e.g., 2022).

La Niña still brings rain — but now it brings chaotic, extreme rain, not the gentle “wet opposite” of El Niño.


🌡️ 4. La Niña droughts are also becoming worse

Even though La Niña tends to be wetter in many regions, it still causes drought in others — and those droughts are now more severe:

The southern U.S. experiences deeper drought.

South America (especially Argentina) sees agricultural collapse.

East Africa suffered a historic multi‑year drought during La Niña.

Climate change amplifies both sides:

Wetter regions get wetter.

Drier regions get drier.

So the “opposite” pattern is still there, but more violent and less predictable.


🌍 5. ENSO’s global influence is changing

ENSO (El Niño–La Niña) used to be the dominant driver of year‑to‑year climate variability.

Now:

Climate change is the dominant driver.

ENSO events ride on top of a much warmer baseline.

Their effects are amplified, distorted, or overridden.


This means:

La Niña still cools the planet a little, but not enough to counteract warming.

La Niña still brings rain to Asia, but often too much.

La Niña still brings drought to the Americas, but more severe.


🎯 Bottom line

Yes — La Niña still brings the opposite effects of El Niño.

But climate change is making those effects more extreme, less predictable, and less symmetrical.

The “pendulum” still swings, but the whole system is now tilted by global warming.


If you want, I can also explain:

Why ENSO events may be getting stronger

How El Niño and La Niña affect Europe specifically

What a future “super La Niña” might look like

Just tell me which direction you’d like to explore.


                                                            *     *     *

So there we have it; our overview. ENSO (the El Nino/La Nina cycle) is the mechanism through

which temperatures on the Pacific Coast of Eurasia and that of the Americas normalize. For us, hotter

water from Asia ends up on the US coast(El Nino); cooler water from North America reaches

 Asia (El Nina)!






Tjere

Solutions...

 Gemini AI:

Climate; how come Europe is experiencing drought conditions this summer. Granted the air is warmer, but there are still trees and crops on the ground...

The paradox you are pointing to—that a region can be suffering from severe drought even while trees and crops are physically still standing in the fields—highlights how modern agricultural and ecological droughts work.  

A drought is not merely a sudden disappearance of all plant life; rather, it is a water deficit crisis driven by a compounding cycle of atmospheric conditions.  

World Weather Attribution


1. The "Thirsty" Atmosphere (Potential Evapotranspiration)

While people often think of drought solely in terms of a lack of rain, scientists measure it heavily through evaporative demand. When air temperatures spike:  

Warm air acts like a giant sponge. It dramatically increases the atmosphere's "thirst," rapidly pulling moisture directly out of soils, lakes, reservoirs, and vegetation.  

Even if some rain fell earlier in the year, soaring temperatures cause surface water to evaporate at an accelerated rate long before it can replenish deep soil moisture.  


2. Why the Trees and Crops Are Still Standing (For Now)

Plants and trees are remarkably resilient survivors, but they pay a heavy physiological price during heatwaves:

Stressing, not thriving: Just because crops and trees are "on the ground" doesn’t mean they are healthy. When the air becomes searingly hot and dry, plants try to protect themselves by closing tiny pores (stomata) to prevent water from evaporating out of their leaves.

Shutting down growth: By closing these pores, plants stop taking in carbon dioxide efficiently, which stunts their growth, turns leaves brittle or brown, and causes yields to wither long before the plant actually dies.

Depleting deep reserves: Perennial trees can survive initial dry spells by pulling moisture from deep root systems. However, when a drought stretches across multiple months or years, those deep water tables drop out of reach, leaving trees vulnerable to disease, pests, and eventual die-off.


3. The Runoff Problem

When it does rain during these climate patterns, it often comes down in sudden, heavy downpours rather than steady absorption. Because prolonged heat baked the soil hard and dry, the ground loses its ability to soak up water efficiently. Instead of penetrating the earth to replenish groundwater, the water runs off the surface, triggering flash floods while leaving the underlying soil just as parched as before.  

Ultimately, Europe's summer droughts are less about the complete absence of vegetation and much more about an invisible, aggressive drying out of the soil and water systems that those plants and crops rely on to actually produce a harvest.  

                                                           *     *     *

https://share.gemini.google/xuJDVctscDZi


Sunday, August 16, 2026

R_Cultivation

Italian Rice Cultivation:

https://share.gemini.google/Q1J4T899Y3mk

                                                                                 


Piedmont (Turin)

Liguria (Genoa)


Lombardi (Milan)

Lombardy[b] (Lombard and Italian: Lombardia;[a][c] Romansh: Lumbardia) is an administrative region of Italy that covers 23,844 km2 (9,206 sq mi); it is located in northern Italy and with a population of about 10 million is the most populous region, constituting more than one-sixth of Italy's population. Lombardy is located between the Alps mountain range and tributaries of the river Po, and includes Milan, its capital and largest city, whose metropolitan area is the largest in the country and among the largest in the EU.

...Lombardy is one of the main European regions for rice production and together with Piedmont, produces 93% of Italian rice.





Drought_2026

 https://archive.ph/aHEnx

Copilot:

European Drought; since when has Italy been growing rice!??

Italy has been growing rice for centuries — long before modern droughts, climate change, or even the unification of Italy. The Reuters article you’re reading simply reflects how that very old tradition is now under extreme pressure from water scarcity.

Here’s the clear timeline.

🇮🇹 When did Italy start growing rice?

Rice cultivation in Italy began in the late Middle Ages, around the 1400s, and expanded rapidly in the Renaissance. By the 1500s, northern Italy — especially the Po Valley — had become one of Europe’s main rice-growing regions.

This is not new at all. It’s one of the oldest rice cultures outside Asia.


🌾 Why Italy?

Northern Italy’s Po Valley has:

naturally flat floodplains

abundant rivers (Po, Ticino, Sesia)

Alpine snowmelt feeding irrigation canals

a warm summer climate ideal for paddy rice

This combination made it perfect for rice long before modern irrigation engineering.

The Reuters page you’re reading confirms Italy’s current dominance:


Italy is Europe’s largest rice producer 

About 235,000 hectares planted in 2025 

Over 80% grown in Pavia, Vercelli, Novara — the historic rice heartland 

Those provinces have been growing rice for 500+ years.


🧭 Historical milestones

1400s: Rice introduced to northern Italy, likely via Arab influence through Spain.

1500s: Massive canal-building (Navigli, Canale Cavour) expands rice paddies.

1800s: Italy becomes Europe’s top rice producer.

1900s–today: Arborio, Carnaroli, Vialone Nano become iconic risotto varieties.

So when you see “Italy’s rice belt” in the article, it’s referring to a region with half a millennium of rice farming tradition.


🌡️ Why the drought matters so much now

The article shows how climate change is hitting a crop that depends on stable water supplies:

Lake Maggiore in extreme drought 

Po River at record low levels for the season 

Farmers forced to abandon fields and rotate irrigation weekly 

Rice is water‑intensive, so Italy’s centuries-old system is suddenly fragile.


If you want, I can also explain:

why Europe grows rice at all

how Italian rice differs from Asian rice

how drought is reshaping European agriculture

whether Italy might eventually have to give up rice

Just tell me what direction you want to explore next.


Why does Europe grow rice at all?

Europe grows rice for a very simple reason: parts of Europe have the exact climate, soils, and water systems needed for paddy rice — and they’ve had them for centuries. The Reuters article you’re reading even notes that Italy’s rice belt has long thrived on the Po basin , which is the heart of the story.

Here’s the full picture, clearly laid out.


🌾 Why Europe grows rice at all

1. Europe has the right geography in a few key places

Rice needs:

flat floodplains

slow-moving water

warm summers

soils that hold moisture


Northern Italy’s Po Valley is basically a natural rice machine:

huge flat plains

rivers fed by Alpine snowmelt

centuries-old irrigation canals

hot summers

That’s why Italy became Europe’s largest rice producer — 235,000 hectares in 2025 .

Spain’s Valencia and Sevilla regions, and parts of Portugal and Greece, have similar conditions.


2. Rice arrived in Europe early — and stuck

Rice was introduced to Europe in the Middle Ages through:

Arab agriculture in Spain

Mediterranean trade routes

later, Renaissance-era farming innovations

By the 1400s–1500s, Italy and Spain were already major rice-growing regions.

Europe didn’t adopt rice because of Asia — it adopted rice because its own landscapes could support it.


3. Europeans developed their own rice styles

Europe doesn’t grow Asian long-grain rice.

It grows short‑grain, high‑starch varieties perfect for:

risotto

paella

arroz caldoso

rice puddings

These varieties (Arborio, Carnaroli, Vialone Nano, Bomba, Calasparra) became culturally essential foods.

Once a crop becomes part of national cuisine, it becomes economically entrenched.


4. Rice fits Europe’s historic irrigation systems

Italy’s rice belt is built on:

Renaissance canals

Alpine-fed rivers

controlled flooding systems


The Reuters article shows how deeply this infrastructure is woven into farming life:

farmers rotate irrigation weekly to share scarce water 

Alpine snowmelt still keeps irrigation barely possible 

Rice wasn’t a random choice — it was the crop that best matched the water engineering Europe already had.


5. Europe needed a reliable staple crop

Before potatoes arrived from the Americas, rice was one of the few dependable, high-calorie crops that could thrive in wet lowlands.

It became a strategic food source.


🌍 So why does Europe grow rice?

Because certain European regions are naturally suited to it, and once rice became embedded in cuisine, economy, and irrigation systems, it stayed.

The drought you’re reading about is dramatic precisely because rice has been there for 500+ years — and now the water systems that sustained it are breaking down.


If you want, I can go deeper into:

whether Europe might eventually stop growing rice

how climate change is shifting rice production northward

why Italian rice tastes different from Asian rice

how Alpine snowmelt historically powered the entire rice belt

Just tell me what direction you want to explore next.


Is this year's drought in Europe novel, or have there been drougths before. I would think Alpine melt is pretty realiable!!

Europe has absolutely had droughts before — even severe ones — but the drought described in your Reuters tab is unusually intense, unusually early, and part of a clear accelerating trend, not just a random bad year.

And you’re right: Alpine melt used to be reliable. The article itself shows how that reliability is breaking down.

Let me walk you through what’s genuinely new — and what isn’t — using the page you’re reading.


🌍 Europe has had droughts before — but 2026 is different

Historically, Europe’s big drought years include:

1540 (the “Megadrought” — rivers dried up across Europe)

1921

2003

2017

2022 (the worst in 500 years)


So drought is not new.

What is new is the frequency, intensity, and timing.

Your Reuters article explicitly says farmers find 2026 even harder than 2022:

locals say it is proving even harder than the severe drought of 2022 

That’s a big statement, because 2022 was catastrophic.


🏔️ Alpine melt used to be Europe’s water insurance — but it’s failing

This is the key shift.

The Po Valley’s entire rice system depends on:

snowpack

glaciers

slow summer melt

The article confirms that irrigation is only barely possible because glaciers are melting faster:

irrigation remains possible largely because Alpine ice reserves continue to melt as temperatures rise 

But here’s the problem:

1. Snow is melting too early

Farmers are already seeing early melt:

As snow melts earlier in a warming climate… 

Early melt means:

water arrives in spring

fields need it in July–August

by midsummer, rivers and lakes collapse

This is exactly what happened in 2026.


2. Alpine lakes are hitting record lows

The article states:

reserves in the Alpine lakes are running low   

Lake Maggiore is now classified as being in extreme drought conditions 

Lake Maggiore is one of the main water sources for Italy’s rice belt.


3. The Po River hit a record low for the season

water levels in the Po recently fell to a record low for the time of year in Cremona 


The Po is the backbone of northern Italy’s agriculture.

A seasonal record low is a major red flag.


🔥 What makes 2026 “novel”?

1. The drought severity level is officially “high”

The Po River Basin Authority issued a high drought severity warning:

high level of drought severity… reserves running low 


2. Farmers had to adopt an unprecedented irrigation rotation

This has never been done before:

“This year, we had to introduce a rotation system”   

 Under the scheme, different sections receive water in alternating weeks, allowing scarce resources to be shared ‌across ...

That’s a sign of extreme scarcity.


3. Entire fields were abandoned

fields… left without water for weeks, never reached maturity   

he decided to channel all available water to part of his land, abandoning the remaining plots Current pageCurrent page. To avoid jeopardising the entire harvest, he decided to channel all available water to part of his land, abandoning the ...

This is not normal drought management — it’s triage.


4. Farmers are considering reviving medieval techniques

Winter flooding — a practice largely abandoned decades ago — is being reconsidered:

farmers are discussing reviving practices… such as winter flooding 

When modern irrigation fails, farmers look backward.


🧭 So is Alpine melt still reliable?

Short answer: no — not anymore.

The article makes this clear:

Alpine melt still exists

but it’s arriving too early

and it’s not enough to sustain summer irrigation

The Po Valley was “long accustomed to abundant water supplies”:

Long accustomed to abundant water supplies… Italy’s rice belt has been forced to adopt an unprecedented response 

That line captures the shift perfectly.


🧩 Bottom line

Europe has always had droughts.

But the 2026 drought is part of a new pattern: earlier snowmelt, hotter summers, lower rivers, and water systems pushed beyond their design limits.

Alpine melt used to be a guarantee.

Now it’s a warning sign.


If you want, I can also explain:

why Alpine snowmelt is collapsing

how Europe’s rivers (Rhine, Danube, Loire) are changing

whether Italy might eventually have to abandon rice

how drought is reshaping European food security

Just tell me where you want to go next.

                                                                                        

                        

                                            image source: Wikipedia