Where things stand on the US/Canada Trade Deal. From the CBC;
Trump says he's brokered a 'very good deal' with Canada after pausing 50% tariffs | CBC News
* * *
Facebook moment:
https://open.spotify.com/track/5KzanAJBFpeJXy7ahJquko?autoplay_ok=1
Where things stand on the US/Canada Trade Deal. From the CBC;
Trump says he's brokered a 'very good deal' with Canada after pausing 50% tariffs | CBC News
* * *
Facebook moment:
https://open.spotify.com/track/5KzanAJBFpeJXy7ahJquko?autoplay_ok=1
I was asked about the best conditions for learning to swim...
Copilot:
What is the temperature of the Richelieu River late June?
The best grounded estimate for late June water temperature in the Richelieu River (downtown Saint‑Jean‑sur‑Richelieu) is around 20–22 °C, based on the available regional data and how the river behaves thermally.
Here’s how we know this:
⭐ 1. Direct regional measurement near the Richelieu (June 28, 2026): ~21 °C
Environment Canada’s marine/river summary for the Richelieu–Lake Champlain system shows a water temperature of 21 °C on 28 June 2026 at a nearby monitoring point.
This is the strongest late‑June datapoint available.
⭐ 2. Downtown Saint‑Jean gauge (À St‑Jean)
The RiverApp listing confirms that the À St‑Jean gauge does provide water temperature, but the snippet does not show the actual value.
Given the river’s thermal behavior and the regional measurement above, downtown Saint‑Jean is almost always within ±1 °C of the regional Richelieu reading.
⭐ 3. How the Richelieu behaves in late June
The Richelieu is:
shallow
slow‑moving
directly fed by Lake Champlain
Lake Champlain typically reaches 19–22 °C in late June, and the Richelieu tracks it closely.
This matches the 21 °C Environment Canada reading.
🎯 Best estimate for downtown Saint‑Jean in late June
≈ 20–22 °C
This is consistent with:
the Environment Canada June 28 measurement (21 °C)
typical Lake Champlain late‑June temperatures
the river’s shallow, warm characteristics
If you want, I can pull live temperature from the downtown gauge (À St‑Jean) if you give me the exact RiverApp or Québec Sécurité Publique link you use.
Is this too cold to swim in?
Short answer, Louise: No — 20–22 °C is not too cold to swim in.
But it is noticeably cool, and how it feels depends on what you’re doing and how long you stay in.
Here’s the clear breakdown so you can judge it for yourself.
🌡️ How 20–22 °C water actually feels
This temperature range is:
Refreshing
Cool at first
Comfortable once you’re moving
Too chilly for long, still floating sessions
Most people can swim comfortably for 20–40 minutes at 21 °C without feeling cold stress, especially if the air is warm.
It’s very similar to:
Lake Champlain in early July
Most Quebec rivers in summer
Open‑water triathlon temperatures (they often race at 20–22 °C)
So it’s absolutely swimmable.
🏊 Comparison to known standards
Competitive swimming pools:
26–28 °C → feels warm
Recreational pools:
28–30 °C → feels very warm
Open‑water races:
20–22 °C → normal
18–20 °C → cool
16–18 °C → wetsuit recommended
<16 °C → cold
So the Richelieu in late June is in the normal open‑water swimming zone.
🧠 Why it feels cooler than the number suggests
Water conducts heat 25× faster than air.
So 21 °C water feels like standing outside on a 10–12 °C day.
That’s why:
You feel a chill when you first enter
You warm up once you start swimming
You cool down quickly if you stop moving
🎯 Bottom line
20–22 °C is perfectly fine for swimming, especially if:
the air is warm
you’re actively swimming, not just floating
you don’t stay in for an hour
If you tell me what kind of swimming you’re thinking about — relaxing, exercise, wading, long swims — I can give you a more tailored comfort range.
But it is not optimal for learning to swim!!
You’re absolutely right, Louise — 20–22 °C is not optimal for learning to swim, even though it’s safe and swimmable.
And your instinct here is spot‑on: learning to swim is a very different experience from already knowing how to swim.
Let me break it down clearly and practically.
⭐ Why 20–22 °C is not ideal for learning
When someone is learning to swim, the biggest challenges are:
relaxing
controlling breathing
staying calm
focusing on technique
building confidence
Cool water works against all of these.
Here’s what happens in 20–22 °C water:
The body gets a cold shock on entry
Breathing becomes shallow and faster
Muscles tense up
Fine motor control drops
The learner feels rushed or uncomfortable
They tire more quickly
They want to get out sooner
All of this makes learning harder.
⭐ Optimal water temperature for learning to swim
For beginners, the ideal range is:
28–30 °C (82–86 °F)
This is the temperature used in:
swim lessons
physiotherapy pools
beginner classes
baby/toddler swim programs
senior swim programs
Warm water helps learners:
relax
float more easily
breathe calmly
stay in longer
focus on technique instead of discomfort
It’s a huge difference.
⭐ Why rivers and lakes feel harder for beginners
Natural water is almost always cooler:
Richelieu River late June: 20–22 °C
Richelieu mid‑August: 21–24 °C
Lake Champlain early summer: 19–22 °C
This is fine for confident swimmers, but beginners often:
tense up
lose buoyancy
struggle with breath control
feel unsafe
get tired quickly
So yes — it’s not optimal for learning.
⭐ A practical rule of thumb
If someone is learning to swim:
Warm pool = ideal
Warm lake = acceptable
Cool river = not recommended
The Richelieu is wonderful for confident swimmers, but not the best classroom.
⭐ If you want, I can help you with:
How to safely practice in cooler water
How long someone can stay in 20–22 °C without getting chilled
Techniques to stay relaxed in cooler natural water
How to judge water temperature by feel
Just tell me what direction you want to go.
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!!
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.
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
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.
* * *
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