4 Billion Years On

Laos – Sep 2026

September 2026 brought elevated temperatures and severe monsoon disruption across Laos, where persistent heavy rainfall triggered widespread flash flooding that affected over 400,000 people across 16 provinces…

Top 5 Cities: Vientiane, Savannakhet, Pakse, Luang Prabang, and Thakhek

Summary

September 2026 brought elevated temperatures and severe across Laos, where persistent heavy rainfall triggered widespread flash flooding that affected over 400,000 people across 16 provinces. The warm conditions coincided with a strong El Niño forecast to peak at Very Strong in Sep-Nov, tracked at ENSO. While global temperatures hit near-record highs during the period, Laos maintained an average temperature of 24.88°C, sitting 1.0°C above its long-term baseline, with drier conditions anticipated as tropical Pacific warming peaks over the coming months.

This month in numbers

Laos recorded an average temperature of 24.88°C in September 2026, marking a 1.0°C anomaly above the 1961–1990 baseline. This ranked as the 13th warmest month of its kind in 87 years of records, while the broader July–September season averaged 24.95°C (0.8°C above baseline) to rank 14th warmest. Across the globe, land temperatures reached 13.63°C during September (+1.9°C above baseline) to rank as the 2nd warmest on record. The global 3-month average for July–September reached 15.04°C (+1.8°C above baseline), marking the 3rd warmest such period on record.

What changed

While long-term warming has raised Laos's baseline temperatures by 1.22°C compared to 1961–1990, recent months have hovered closer to modern averages following the record-breaking heat of 2024, which reached 24.21°C. Across the broader Asia continent, tracked at Asia, the regional mean anomaly for September reached +1.78°C, placing Laos 0.76°C cooler than its continental peers. On a global scale, Laos sat 201st out of 232 tracked regions for 1-month temperature anomaly and 218th for the 3-month window, reflecting relatively muted thermal anomalies compared to northern high-latitude and Mediterranean hotspots.

What’s driving change?

The primary climate influence across Southeast Asia remains ENSO, with a strong El Niño actively modulating tropical weather patterns as tracked at ENSO. While El Niño classically brings drier conditions to mainland Southeast Asia during the dry season, the transition period frequently induces , altering the timing and intensity of rainfall belts. During September, an active low-pressure trough interacting with the southwest monsoon brought heavy, concentrated rain events rather than evenly distributed precipitation. This erratic moisture delivery triggered major flash flooding across 16 Lao provinces, even as overall monthly temperatures remained modestly elevated.

Looking ahead

With tropical Pacific sea surface temperatures forecast to reach a Very Strong El Niño peak over the coming months, seasonal outlooks suggest a transition toward drier and warmer conditions across Laos as the dry season establishes itself through early next year.

Generated by Gemini from climate data and web sources

At a Glance

Temperature – Average

Laos
Global
Land + Ocean
Sep
+1.2°C· 13th
24.9°C
+1.2°C· 2nd
16.3°C
Record
25.5°C (2017)
16.4°C (2023)
Jul–Sep
+1.0°C· 14th
24.9°C
+1.1°C· 1st
16.7°C
Record
25.6°C (2020)
16.7°C (2026)
2025
+0.8°C· 16th
23.2°C
+1.0°C· 3rd
15.0°C
Record
24.2°C (2024)
15.2°C (2024)
Headline: anomaly vs your baseline (1961–1990 where the record is too short) · small figure: actual value · Record: the record for the ranking above

Climate Insights – Laos

Precipitation, Sunshine, Frost and Snow are converted to standard deviations from their own average so they can share an axis with Temperature anomalies.

Temperature
10-Yr AverageActual Year

Climate History

1912Volcanic

Novarupta (Katmai) eruption

The largest volcanic eruption anywhere in the world in the 20th century - 13 km3 of magma, about thirty times the 1980 Mount St. Helens eruption - at Novarupta in Alaska on 6-8 June 1912. Ash reached 100,000 ft and cooled the Northern Hemisphere by roughly 0.3°C over 1912-13. Unlike a tropical eruption such as Pinatubo, a high-latitude eruption's haze stays in its own hemisphere, so it did little to the Southern Hemisphere.

Smithsonian Global Volcanism Program, Alaska Volcano Observatory, National Park Service, Oman et al. 2005

1945Industrial Aerosol

Post-WWII industrial expansion begins

After the Second World War, coal and oil use grew rapidly across Europe, North America and the Soviet Union. Global sulphur dioxide emissions rose from about 30 to about 130 million tonnes a year by 1980, and the sulphate haze they formed masked part of the greenhouse warming underneath - the effect known as 'global dimming'.

Klimont et al. 2013

1950-2025ENSO

How much ENSO really controls Laos's climate

ENSO matters in Laos, most of all in March-May: the El Niño-La Niña cycle explains about 33% of the year-to-year swing in Laos's March-May rainfall, with El Niño years tending drier and La Niña years wetter. That puts Laos among the 88 countries in this site's data where ENSO's influence is strong enough to be worth reporting.

NOAA CPC

1955-56ENSO

The 1955-56 La Niña

Laos's rainfall for March-May 1956 ran +24% against its 1961-90 average - the wet March-May that La Niña usually brings here.

ONI -1.6°C · RONI -1.4°C

NOAA CPCENSO Tracker

1958GHG Milestone

Keeling Curve begins

Charles David Keeling begins continuous measurements of atmospheric CO₂ at Mauna Loa Observatory in Hawaii, starting at about 315 ppm. The record has risen every year since and is now the longest unbroken direct measurement of CO₂ anywhere - the 'Keeling Curve'.

NOAA GMLGreenhouse Gases

1963Volcanic

Agung eruption

Agung's eruption in Bali put a veil of sulphate haze into the stratosphere that cooled global temperature by about 0.3°C over 1963-66.

Smithsonian Global Volcanism Program, NOAA Global Monitoring Laboratory

1973-74ENSO

The 1973-74 La Niña

Laos's rainfall for March-May 1974 ran +26% against its 1961-90 average - the wet March-May that La Niña usually brings here.

ONI -2.0°C · RONI -1.9°C

NOAA CPCENSO Tracker

1977Ocean Oscillation

Pacific Decadal Oscillation flips to a warm phase

The Pacific Decadal Oscillation - a slow natural cycle in North Pacific sea temperatures - switches from its cool to its warm phase in 1976-77. The change was abrupt enough to be called the 1976-77 Pacific Climate Shift: it warmed Alaska and the west coast of North America, and reorganised North Pacific fisheries.

Learn more →

1979Industrial Aerosol

Global SO2 emissions peak

Global sulphur dioxide emissions peak at about 130 million tonnes a year, then begin a long decline as Europe, North America and Japan clean up their air. As the aerosol mask thins, the rate of global warming picks up through the 1980s.

Klimont et al. 2013

1982Volcanic

El Chichón eruption

A sulphur-rich eruption in Mexico whose aerosol cloud stayed in the stratosphere for more than two years, cooling the Northern Hemisphere by about 0.2°C.

Smithsonian Global Volcanism Program

1982-83ENSO

1982-83 El Niño

Laos's rainfall for March-May 1983 ran -20% against its 1961-90 average - the dry March-May that El Niño usually brings here. On NOAA's Relative Oceanic Niño Index this is the strongest El Niño since 1950.

ONI +2.1°C · RONI +2.4°C

NOAA CPC, NOAA CPC (2)ENSO Tracker

1985Other

The Antarctic ozone hole is discovered

British Antarctic Survey scientists Joe Farman, Brian Gardiner and Jon Shanklin publish their Halley and Faraday measurements on 16 May 1985, showing October ozone over Antarctica had fallen to about two-thirds of earlier decades. The cause is traced to chlorofluorocarbons, and the finding triggers the fastest international environmental response on record.

Nature, UKRI

1987Other

The Montreal Protocol

Signed in 1987 to phase out ozone-depleting chlorofluorocarbons, the Montreal Protocol turned out to be one of the most consequential climate treaties ever agreed. CFCs are potent greenhouse gases in their own right, and NOAA estimates the Protocol prevented up to 2°C of warming by 2100 - around 1°C from the emissions avoided, and up to 1°C more by sparing forests and other carbon sinks from increased ultraviolet radiation.

NOAA, Wikipedia

1988GHG Milestone

CO₂ crosses 350 ppm

Atmospheric CO₂ passes 350 ppm. In the same year James Hansen told a US Senate committee that global warming was already detectable, the moment it entered mainstream politics. Twenty years later, in 2008, Hansen proposed 350 ppm as the safe upper limit - a level the world had already left behind.

NOAA GMLGreenhouse Gases

1988-89ENSO

The 1988-89 La Niña

Laos's rainfall for March-May 1989 ran +14% against its 1961-90 average - the wet March-May that La Niña usually brings here.

ONI -1.9°C · RONI -1.9°C

NOAA CPCENSO Tracker

1990Pattern Shift

Daytime warming catches up with the night-led pattern

Across 1961-90, 81% of the world's land saw nights warming faster than days. Across 1991-2020 the pattern reversed: 70% saw days warming faster, as the industrial haze that had been dimming daytime sunshine was cleaned up. The study compares two fixed thirty-year windows; measured as a turning point, this site's own global series turns around 1982.

Zhong et al. 2023

1991-93Volcanic

Mount Pinatubo erupts

Pinatubo's cooling is only faintly visible in Laos's own record. 1992, the year after the June 1991 eruption, ranks 29th-coldest of the 76 years there. A single large eruption can hold temperatures down for two or three years; it cannot reverse the trend.

Learn more →

1995Ocean Oscillation

Atlantic Multidecadal Oscillation flips to a warm phase

The Atlantic Multidecadal Oscillation - a slow natural cycle in North Atlantic sea temperatures, roughly 60-70 years long - flips to its warm phase in 1995. Warm phases are linked to more active Atlantic hurricane seasons, wetter summers in parts of north-west Europe and more frequent drought in the central and western United States.

Learn more →

1997-98ENSO

1997-98 El Niño

One of the strongest El Niños on record, and the one the textbook El Niño pattern is usually drawn from. It pushed 1998 to what was then the warmest year ever measured, and set off the first global-scale coral bleaching event.

ONI +2.4°C · RONI +2.3°C

NOAA CPC, NOAA NCEIENSO Tracker

1999-2001ENSO

The 1999-2001 La Niña

Laos's rainfall for March-May 2000 ran +23% against its 1961-90 average - the wet March-May that La Niña usually brings here.

ONI -1.5°C · RONI -1.6°C

NOAA CPC ONI

1999Ocean Oscillation

Pacific Decadal Oscillation flips back to a cool phase

The Pacific Decadal Oscillation - a slow natural cycle in North Pacific sea temperatures - flips back to its cool phase around 1998-99. The cool phase that followed is one reason global surface warming appeared to slow in the 2000s, as more heat went into the deep Pacific.

Learn more →

2007-08ENSO

The 2007-08 La Niña

Laos's rainfall for March-May 2008 ran +13% against its 1961-90 average - the wet March-May that La Niña usually brings here.

ONI -1.8°C · RONI -1.7°C

NOAA CPCENSO Tracker

2009-10ENSO

2009-10 El Niño

Laos's rainfall for March-May 2010 ran -26% against its 1961-90 average - the dry March-May that El Niño usually brings here. 2010 is also Laos's 8th-warmest year in this site's 1950-2025 record.

ONI +1.5°C · RONI +1.5°C

NOAA/IRI ENSO archiveENSO Tracker

2010Pattern Shift

Global heatwave days sharply accelerate

Laos's own heatwave days - days in warm spells well above the local norm - rose from a 1961-90 average of 3.4 a year to 27.1 in 2016-25 - 8 times as many. Worldwide, heatwave days have roughly doubled each decade since 2010, as the whole temperature distribution has shifted upwards.

Learn more →Heatwave Days

2010-12ENSO

The 2010-2012 La Niña

Laos's rainfall for March-May 2011 ran +12% against its 1961-90 average - the wet March-May that La Niña usually brings here.

ONI -1.6°C · RONI -1.6°C

NOAA CPC ONI

2013GHG Milestone

CO₂ crosses 400 ppm

Atmospheric CO₂ passes 400 ppm at Mauna Loa on 9 May 2013 - a level the planet had not seen for 3-5 million years, since the Pliocene, when sea levels were many metres higher.

NOAA GMLGreenhouse Gases

2015-16ENSO

2015-16 El Niño

Laos's rainfall for March-May 2016 ran -23% against its 1961-90 average - the dry March-May that El Niño usually brings here. By the raw ONI index it was the strongest El Niño ever measured - a reminder that a strong index does not guarantee a strong local outcome.

ONI +2.6°C · RONI +2.3°C

NOAA CPCENSO Tracker

2015-25Pattern Shift

2015-2025: the eleven warmest years on record

Globally, the eleven warmest years on record have all happened since 2015. Laos follows it closely: eight of its own eleven warmest fall in that span, with 2012, 2010 and 1998 outside. Its warmest year is 2024.

Learn more →

2018Flood

The Attapeu dam collapse, 2018

After days of heavy monsoon rain, a saddle dam of the unfinished Xe Pian-Xe Namnoy hydropower project in southern Laos gave way on the night of 23 July 2018. The flood swept through 19 villages in Attapeu province, killing 71 people and displacing about 14,400, and carried on across the border into northern Cambodia.

Wikipedia, NPR

2020GHG Milestone

COVID-19 lockdowns - CO₂ emissions dip

Global fossil CO₂ emissions fell about 5.8% in 2020, from 37.0 to 34.8 billion tonnes, yet atmospheric CO₂ still rose 2.5 ppm - the dip barely registers in the atmospheric record. Emissions were back to pre-pandemic levels by 2022.

Le Quéré et al. 2020

2020Industrial Aerosol

Low-sulphur shipping fuel rule (IMO 2020)

New international shipping rules cut the sulphur allowed in ship fuel from 3.5% to 0.5% almost overnight, removing about 8 million tonnes of sulphur dioxide a year. With less sulphate haze over the oceans, it may have added around 0.1°C of warming by 2023-24.

Gettelman et al. 2024

2023-24ENSO

2023-24 El Niño

Laos's rainfall for March-May 2024 ran -10% against its 1961-90 average - the dry March-May that El Niño usually brings here. Globally it helped produce the record temperatures of 2023 and 2024.

ONI +2.0°C · RONI +1.4°C

NOAA CPCENSO Tracker

Data: Our World in Data / NOAA (precipitation: GPCC (DWD); frost: World Bank CCKP).

Heatwave Days – Laos

Warm Spell Duration Index (WSDI) - days in a 6+ day run above the local 90th-percentile temperature for that time of year.

Heatwave days per year2019 (Record)10-yr avg

Data: World Bank Climate Change Knowledge Portal (ERA5-derived). Refreshed roughly 1-2x/year, ~7-8 months behind present.

Climate Map – Global

Source: Copernicus ERA5 (countries) · NOAA Climate at a Glance (continents, US states & climate regions) · Met Office (UK) · GPCC (rainfall, snow) · World Bank CCKP (frost). Anomalies are vs the 1961–1990 baseline. See methodology.

Year-on-Year Trends

The 4byo Climate Helix – Laos

1940→20261961–1990 baselineColdest (1940)2016–2025 meanWarmest (2024)2026 so far
2026Sep
WetDryJanFebMarAprMayJunJulAugSepOctNovDecWet Start+1 daysWet End~0 days15°20°25°
Temp
24.3°C
+1.9 vs base
Precipitation
1,005mm
-836 vs base
Frost
—
ENSO
—
RONI 3-mo mean
Playback
8×

Data: Our World in Data / NOAA (precipitation: GPCC (DWD); frost: World Bank CCKP).

Monthly Temperature – Laos

All years since 19402024 (Warmest)1940 (Coldest)2026 (Current Year)

Background lines: the last 40 years.

Data: Our World in Data / NOAA (precipitation: GPCC (DWD); frost: World Bank CCKP).

Records – Laos

Latest data Sep 2026
Warmest year
2024
24.2°C
Coldest year
1940
21.5°C
2026 so far
#7/87
24.3°C

Our World in Data / NOAA (precipitation: GPCC (DWD); frost: World Bank CCKP) - Anomalies vs 1901-2000 mean

Typical Climate – Laos

Köppen Aw · Tropical

Laos has a tropical climate (Köppen Aw: Tropical savanna (dry winter)), with both a warm/cold cycle and a wet/dry cycle through the year. May is typically the warmest month, averaging 26.2°C, while January is the coldest at 19.3°C. Annual precipitation averages around 1919mm, concentrated mostly in the wet season.

Warmest month
May 26°C
Coldest month
Jan 19°C
Annual rainfall
1919mm
Wettest month
Jul 387mm

Monthly climate normals (2016–2025) - bar colour and height show average temperature, the shaded area shows average monthly precipitation.

Data: Our World in Data / NOAA (precipitation: GPCC (DWD); frost: World Bank CCKP).

Shifting Seasons

Warm/cold + wet/dryKöppen Aw · Tropical

Laos has both a clear warm/cold cycle (±3.1°C) and a wet/dry cycle (20× wet:dry ratio). Both sides of the annual rhythm are shown below.

Shifting summer
39 days Longer
Warm Season
1940–1969 Baseline: 9 Mar → 17 Oct · 223 days
2016–2025 Now: 27 Feb → 16 Nov · 262 days
−10d
+30d
J
F
M
A
M
J
J
A
S
O
N
D
Spr 9 days EarlierAut 30 days Later
Shifting wet season
1 day Shorter
Wet Season
1891–1920 Baseline: 10 Jun → 5 Sept · 87 days
2016–2025 Now: 11 Jun → 5 Sept · 85 days
+1d
0d
J
F
M
A
M
J
J
A
S
O
N
D
Onset 1 day Later
+2.6% annual rain
baseline avgrecent avgClick a marker for each decade
Wet-season onset
10 Jun→11 Jun
1 day Later
When 25% of annual rain has fallen
Wet-season end
5 Sept→5 Sept
no change
When 75% of annual rain has fallen
Peak-rain month
Aug→Jul
-1 month
Wet months: 5 → 5
1891–19202016–2025Wet-month threshold (156 mm)

Monthly precipitation climatology. A “wet month” exceeds the baseline monthly mean (dashed gold line). Biggest month-to-month shift: Jul (+33 mm, +9%).

Data: Our World in Data / NOAA (precipitation: GPCC (DWD); frost: World Bank CCKP).

Extreme Weather

Alerts & Disasters - Laos

Live GDACS alerts in Laos - Red (Major), Orange (Severe) or Green (Moderate) - and the long-term record of weather and climate disasters.

Live Alerts

Loading…

Alerts, Last 12 Months

Major

1

0.8 a year since 2021

Severe

2

1.3 a year since 2021

Moderate

99

Weather Disasters in 2025 - Latest Complete Year

Disasters

2

1.8 a year, 2016-2025

Deaths

15

20 a year, 2016-2025

Weather Disasters, 2016-2025

Most Frequent

Storms & Cyclones

9 of 18 disasters

Deadliest

Flood

181 of 198 deaths

Disasters: EM-DAT, CRED / UCLouvain, via Our World in Data - 10+ deaths, 100+ people affected, or a declared emergency or call for international help. Alerts: GDACS.

Climate Drivers

Climate Drivers - Laos

The natural climate patterns that measurably shape seasonal temperature or rainfall in Laos, from this site’s own data since 1950 - long-term trends removed, and ENSO’s share taken out before scoring the others, so each is credited only for what it adds.

El Niño / La Niña (ENSO)strong link

The tropical Pacific’s warm and cool swings - the biggest natural driver of year-to-year climate.

Now: El Niño (strong) · RONI +1.7°C (Jul-Sep 2026)

Forecast - 100% very strong at peak, Sep-Nov, then neutral by Apr-Jun 2027 (NOAA). La Niña from Sep 2027 in SNU’s AI model.

Strongest in Mar-May rainfall: El Niño tends to bring drier conditions here, La Niña the reverse (about 33% of year-to-year variation).

ENSO Tracker

Emissions & Energy

Explore

Explore Climate Data

Data Sources

Data Sources for Laos

Every figure on this page is sourced from official, openly published climate datasets. Anomalies are calculated against the 1961–1990 baseline (temperature) and 1991–2020 (rainfall, sunshine, frost) - see the Methodology & Sources page for the complete dataset list and update calendar.

FAQs

FAQs

How is the climate in Laos changing?

Laos is warming in line with the rest of the world. The page above shows the latest monthly temperature anomaly versus the 1961-1990 baseline, the long-term annual trend, and the region's rank in the historical record. The headline panel also shows the long-term trend rate per decade and the warmest and coolest years on file.

What is the climate like in Laos?

Laos has a tropical climate (Köppen Aw: Tropical savanna (dry winter)), with both a warm/cold cycle and a wet/dry cycle through the year. May is typically the warmest month, averaging 26.2°C, while January is the coldest at 19.3°C. Annual precipitation averages around 1919mm, concentrated mostly in the wet season.

Which climate drivers affect the weather in Laos?

Measured from seasonal temperature and rainfall in Laos since 1950, with the long-term warming trend removed (and ENSO's own share removed before scoring the other drivers), the climate drivers with a clear effect here are: El Niño / La Niña (ENSO) - strong, strongest in Mar-May rainfall, which El Niño tends to make drier here (La Niña the reverse), about 33% of year-to-year variation. Their current state is shown in the Climate Drivers section of this page.

What extreme weather affects Laos?

In 2025, the latest complete year, the international disaster database EM-DAT recorded 2 weather and climate disasters in Laos, against an average of 1.8 a year in 2016-2025, with 15 deaths. Over those ten years the most frequent type was storms & cyclones (9 of 18) and the deadliest flood. GDACS, the UN and European Commission's disaster alert system, issued 1 Major (Red) and 2 Severe (Orange) alerts for Laos in the last 12 months. Live alerts are on this page and on the Extreme Weather tracker.

Where does the climate data for Laos come from?

Climate data for Laos comes from Our World in Data, sourcing Copernicus ERA5 and HadCRUT5 (national temperature anomaly) and the Global Carbon Project via Our World in Data (CO₂ emissions), refreshed every month, when the upstream temperature and rainfall data are refreshed.

What is the climate baseline used on this page?

Anomalies on this page are calculated against the 1961-1990 climatological baseline, which is the standard reference period used by the Met Office, NOAA, IPCC and most national climate services. Some panels also show the source-native 1901-2000 (NOAA) or 1991-2020 (WMO) baselines for verification. See Methodology & Sources for the full reference.

Which areas does the Laos climate data cover?

The Laos climate profile covers Vientiane, Savannakhet, Pakse, Luang Prabang and surrounding areas. Temperature, rainfall and emissions data for Laos

How often is the Laos climate update refreshed?

The Laos climate update is refreshed monthly, typically a few days after the previous month closes and the upstream provider (Met Office HadUK-Grid, NOAA Climate at a Glance, Copernicus ERA5 or the Global Carbon Project) publishes its update. See the Climate Rankings for cross-region comparisons.

What counts as a Heatwave Day on the Laos climate page?

Heatwave Days use the Warm Spell Duration Index (WSDI) - the WMO/ETCCDI-standard heatwave measure: days that are part of a run of 6 or more consecutive days above the local 90th-percentile temperature for that calendar day. The 90th-percentile threshold varies by time of year (a hot day in January is judged differently to one in July) but is fixed to the 1961-1990 baseline for every year shown - it does not shift as the climate warms, which is why Heatwave Days trend upward over time.

Does the Laos climate page include frost and snow data?

Yes. Frost Days (days with a minimum temperature below 0°C, World Bank CCKP) and snow water-equivalent (GPCC) are shown alongside temperature and precipitation, each measured against the 1961-1990 baseline where a like-for-like historical comparison is available.

What major climate events has Laos experienced?

Major climate events in Laos include The Attapeu dam collapse, 2018; The 1973-74 La Niña; The 1988-89 La Niña; The 1999-2001 La Niña; 2009-10 El Niño; The 2010-2012 La Niña; 2015-2025: the eleven warmest years on record. The Climate History panel on this page lists 32 sourced events and pattern shifts relevant to Laos, the earliest from 1912 - 1 about Laos itself and the rest global context such as volcanic eruptions and El Niño events. Each entry carries its own sources and can be searched, filtered to local events or by category, and sorted by date; scrolling the list moves a cursor across the chart above so you can see where each event falls in the record.

Where does the Climate History list for Laos come from, and how is it checked?

It is a hand-reviewed register, not an automatic feed. Every entry is sourced, and each one records how it was verified - against this site's own data series, against a peer-reviewed paper, or against the public record of the event. 14 of the 32 entries here are written specifically about Laos, usually quoting its own ranking or measured figures. The rest give global or national context shared with wider pages. Where a figure is narrower than it first appears, or a famous claim does not hold locally, the entry says so.