4 Billion Years On

Sri Lanka – Sep 2026

Top 5 Cities: Colombo, Kandy, Galle, Jaffna, and Negombo

Temperature, rainfall and emissions data for Sri Lanka

A fresh climate update for Sri Lanka is being generated…

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At a Glance

Temperature – Average

Sri Lanka
Global
Land + Ocean
Sep
+1.7°C· 1st
28.4°C
+1.2°C· 2nd
16.3°C
Record
28.4°C (2026)
16.4°C (2023)
Jul–Sep
+1.6°C· 1st
28.4°C
+1.1°C· 1st
16.7°C
Record
28.4°C (2026)
16.7°C (2026)
2025
+0.9°C· 6th
26.9°C
+1.0°C· 3rd
15.0°C
Record
27.3°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 – Sri Lanka

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 Sri Lanka's climate

ENSO matters in Sri Lanka, most of all in February-April: the El Niño-La Niña cycle explains about 32% of the year-to-year swing in Sri Lanka's February-April temperatures, with El Niño years tending warmer and La Niña years cooler. That puts Sri Lanka 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

Sri Lanka's temperatures for February-April 1956 ran -0.5°C against the 1961-90 average - the cool February-April 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

1972-73ENSO

The 1972-73 El Niño

Sri Lanka's temperatures for February-April 1973 ran +0.8°C against the 1961-90 average - the warm February-April that El Niño usually brings here.

ONI +1.8°C · RONI +2.0°C

NOAA CPCENSO Tracker

1973-74ENSO

The 1973-74 La Niña

Sri Lanka's temperatures for February-April 1974 ran -0.4°C against the 1961-90 average - the cool February-April that La Niña usually brings here.

ONI -2.0°C · RONI -1.9°C

NOAA CPCENSO Tracker

1975-76ENSO

The 1975-76 La Niña

Sri Lanka's temperatures for February-April 1976 ran -0.3°C against the 1961-90 average - the cool February-April that La Niña usually brings here.

ONI -1.6°C · RONI -1.1°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

Sri Lanka's temperatures for February-April 1983 ran +1.4°C against the 1961-90 average - the warm February-April 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

1986-88ENSO

The long 1986-88 El Niño

1987 is Sri Lanka's 12th-warmest year in this site's 1950-2025 record. The 1986-88 El Niño kept the tropical Pacific warm through the whole of 1987, and temperatures across much of the tropics rose with it.

NOAA CPCENSO Tracker

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

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 does not show in Sri Lanka's own record: 1992, the year after the June 1991 eruption, was an unremarkable year there, 34th-coldest of 76. 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

Sri Lanka's temperatures for February-April 1998 ran +1.8°C against the 1961-90 average - the warm February-April that El Niño usually brings here. It is often treated as the textbook strong El Niño.

ONI +2.4°C · RONI +2.3°C

NOAA CPC, NOAA NCEIENSO Tracker

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

Sri Lanka's temperatures for February-April 2008 ran -0.3°C against the 1961-90 average - the cool February-April that La Niña usually brings here.

ONI -1.8°C · RONI -1.7°C

NOAA CPCENSO Tracker

2009-10ENSO

2009-10 El Niño

Sri Lanka's temperatures for February-April 2010 ran +0.9°C against the 1961-90 average - the warm February-April that El Niño usually brings here.

ONI +1.5°C · RONI +1.5°C

NOAA/IRI ENSO archiveENSO Tracker

2010Pattern Shift

Global heatwave days sharply accelerate

Sri Lanka's own heatwave days - days in warm spells well above the local norm - rose from a 1961-90 average of 11.5 a year to 30.0 in 2016-25 - 3 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

Sri Lanka's temperatures for February-April 2011 ran -0.3°C against the 1961-90 average - the cool February-April 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

Sri Lanka's temperatures for February-April 2016 ran +1.5°C against the 1961-90 average - the warm February-April 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. Sri Lanka follows it closely: seven of its own eleven warmest fall in that span, with 2009, 2005, 1998 and 1983 outside. Its warmest year is 2024.

Learn more →

2016Flood

Cyclone Roanu and the Aranayake landslide, 2016

In mid-May 2016 the storm that became Cyclone Roanu brought days of torrential rain to Sri Lanka. At Aranayake in Kegalle district a hillside collapsed and buried three villages, and across the country floods and landslides killed more than 100 people and displaced over 230,000.

UN News, FloodList

2017Flood

Sri Lanka's monsoon floods, 2017

On 25-26 May 2017 the south-west monsoon, reinforced by the system that became Cyclone Mora, brought torrential rain to Sri Lanka. Floods and landslides hit 15 of the country's 25 districts and killed more than 200 people.

GFDRR, NASA Earth Observatory

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

2020-23ENSO

The 2020-2023 'triple-dip' La Niña

Sri Lanka's temperatures for February-April 2021 ran +0.2°C against the 1961-90 average - the opposite of the cool February-April La Niña usually brings here.

ONI -1.1°C · RONI -1.5°C

WMO, WMO (2)ENSO Tracker

2023-24ENSO

2023-24 El Niño

Sri Lanka's temperatures for February-April 2024 ran +1.5°C against the 1961-90 average - the warm February-April 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 – Sri Lanka

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 year2024 (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 – Sri Lanka

1940→20261961–1990 baselineColdest (1942)2016–2025 meanWarmest (2024)2026 so far
2026Sep
WetDryJanFebMarAprMayJunJulAugSepOctNovDec1891-19202016-25Wet Start−15 days1891-19202016-25Wet End−5 days24°26°28°
Temp
27.3°C
+1.2 vs base
Precipitation
613mm
-1,104 vs base
ENSO
—
RONI 3-mo mean
Playback
8×

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

Monthly Temperature – Sri Lanka

All years since 19422024 (Warmest)1942 (Coldest)2026 (Current Year)

Background lines: the last 40 years.

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

Records – Sri Lanka

Latest data Sep 2026
Warmest year
2024
27.3°C
Coldest year
1942
25.0°C
2026 so far
#6/87
27.3°C

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

Typical Climate – Sri Lanka

Köppen Af · Tropical

Sri Lanka has a tropical climate (Köppen Af: Tropical rainforest), with only modest temperature variation through the year, but a pronounced wet and dry season. June is typically the warmest month, averaging 28.1°C, while January is the coldest at 25.0°C. Annual precipitation averages around 1721mm, concentrated mostly in the wet season.

Warmest month
Jun 28°C
Coldest month
Jan 25°C
Annual rainfall
1721mm
Wettest month
Nov 325mm

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

Wet / dry seasonsKöppen Af · Tropical

Sri Lanka doesn't have a warm/cold cycle - its monthly temperature range is only 3.1°C across the year - but it does have a strong wet/dry cycle (the wettest month gets 5× as much rain as the driest). So we track how the wet season has shifted instead.

Shifting wet season
9 days Longer
Wet Season
1891–1920 Baseline: 6 Jun → 25 Nov · 172 days
2016–2025 Now: 23 May → 20 Nov · 182 days
−15d
−5d
J
F
M
A
M
J
J
A
S
O
N
D
Onset 15 days EarlierEnd 5 days Earlier
-3.3% annual rain
baseline avgrecent avgClick a marker for each decade
Wet-season onset
6 Jun→23 May
15 days Earlier
When 25% of annual rain has fallen
Wet-season end
25 Nov→20 Nov
5 days Earlier
When 75% of annual rain has fallen
Peak-rain month
Nov→Nov
unchanged
Wet months: 3 → 4
1891–19202016–2025Wet-month threshold (148 mm)

Monthly precipitation climatology. A “wet month” exceeds the baseline monthly mean (dashed gold line). Biggest month-to-month shift: May (+69 mm, +53%).

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

Extreme Weather

Alerts & Disasters - Sri Lanka

Live GDACS alerts in Sri Lanka - 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

0

None since 2021

Severe

2

0.3 a year since 2021

Moderate

4

Weather Disasters in 2024 - Latest Complete Year

Disasters

4

4.1 a year, 2015-2024

Deaths

62

74 a year, 2015-2024

Weather Disasters, 2015-2024

Most Frequent

Flood

26 of 41 disasters

Deadliest

Flood

680 of 743 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 - Sri Lanka

The natural climate patterns that measurably shape seasonal temperature or rainfall in Sri Lanka, 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 Oct 2027 in SNU’s AI model.

Strongest in Feb-Apr temperature: El Niño tends to bring warmer conditions here, La Niña the reverse (about 32% of year-to-year variation).

Sri Lanka warms most in the months after an El Niño peaks, as the tropical Indian Ocean warms right across the basin and holds that warmth into the following spring and summer (Xie et al. 2009) - a separate effect from the monsoon rainfall the regional story describes.

ENSO Tracker

Weaker Links

A small signal in one season - easily outweighed by other weather, and possibly partly chance.

Emissions & Energy

Explore

Explore Climate Data

Data Sources

Data Sources for Sri Lanka

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 Sri Lanka changing?

Sri Lanka 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 Sri Lanka?

Sri Lanka has a tropical climate (Köppen Af: Tropical rainforest), with only modest temperature variation through the year, but a pronounced wet and dry season. June is typically the warmest month, averaging 28.1°C, while January is the coldest at 25.0°C. Annual precipitation averages around 1721mm, concentrated mostly in the wet season.

Which climate drivers affect the weather in Sri Lanka?

Measured from seasonal temperature and rainfall in Sri Lanka 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 Feb-Apr temperature, which El Niño tends to make warmer here (La Niña the reverse), about 32% of year-to-year variation. There are also weaker links to the IOD. Their current state is shown in the Climate Drivers section of this page.

What extreme weather affects Sri Lanka?

In 2024, the latest complete year, the international disaster database EM-DAT recorded 4 weather and climate disasters in Sri Lanka, against an average of 4.1 a year in 2015-2024, with 62 deaths. Over those ten years the most frequent type was flood (26 of 41) and the deadliest flood. GDACS, the UN and European Commission's disaster alert system, issued 0 Major (Red) and 2 Severe (Orange) alerts for Sri Lanka in the last 12 months. Live alerts are on this page and on the Extreme Weather tracker.

Where does the climate data for Sri Lanka come from?

Climate data for Sri Lanka 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 Sri Lanka climate data cover?

The Sri Lanka climate profile covers Colombo, Kandy, Galle, Jaffna and surrounding areas. Temperature, rainfall and emissions data for Sri Lanka

How often is the Sri Lanka climate update refreshed?

The Sri Lanka 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 Sri Lanka 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 Sri Lanka 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 Sri Lanka experienced?

Major climate events in Sri Lanka include Cyclone Roanu and the Aranayake landslide, 2016; The 1972-73 El Niño; 1982-83 El Niño; 1997-98 El Niño; Global heatwave days sharply accelerate (2010); 2015-2025: the eleven warmest years on record. The Climate History panel on this page lists 35 sourced events and pattern shifts relevant to Sri Lanka, the earliest from 1912 - 2 about Sri Lanka 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 Sri Lanka 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. 17 of the 35 entries here are written specifically about Sri Lanka, 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.