4 Billion Years On

Djibouti – Sep 2026

Djibouti experienced exceptional heat through late summer, culminating in its 2nd warmest July to September period on record…

Top 5 Cities: Djibouti City, Ali Sabieh, Dikhil, Tadjourah, and Obock

Summary

Djibouti experienced exceptional heat through late summer, culminating in its 2nd warmest July to September period on record. The latest month registered an average temperature of 32.9°C, making it the 4th warmest September since records began in 1940. The sustained high temperatures have intensified water shortages across the Horn of Africa, contributing to an Orange-level drought tracked on our live map at Extreme Weather tracker. The conditions are being driven in part by a strong El Niño forecast to peak at Very Strong in Sep-Nov, with volatile weather patterns expected in the coming months.

This month in numbers

In September 2026, Djibouti recorded an average temperature of 32.9°C, which sits 2.3°C above the 1961-1990 baseline. This was the 4th warmest month for that time of year in 87 years of record-keeping, coming within 1.09°C of the all-time record set in 2023. Over the broader three-month season from July to September, the nation averaged 34.11°C, marking a 2.6°C positive anomaly that ranks as the 2nd warmest such period on record. Globally, land temperatures during the latest month were also exceptionally high, placing 2nd warmest on record with a 1.9°C anomaly.

What changed

The high three-month anomaly of +2.6°C places Djibouti 47th warmest out of 232 countries and regions tracked globally for the July to September window. Across the African continent, tracked at Africa, Djibouti ran notably hot during the latest month, with its +2.3°C anomaly exceeding the regional average by 0.51°C. This continues a broader long-term trajectory for the country, where average temperatures have risen by 1.12°C above historical baselines, following a warm 2025 that ranked as Djibouti's 3rd warmest year on record at 29.07°C.

What’s driving change?

The elevated heat and dry conditions are driven by and , mechanisms that suppress evaporative cooling across the country's arid landscape. Ocean drivers are also playing a central role, led by a strong El Niño in the tropical Pacific, tracked at ENSO, which historically elevates local temperatures and destabilises seasonal rain patterns. This is further reinforced by a positive Indian Ocean Dipole. An Orange-level drought active from late June to mid-October has severely affected local pasture and water resources, as tracked at Extreme Weather tracker. All of Djibouti's 1 drought this year has happened in the past month.

Looking ahead

With a 100% probability of El Niño continuing through the winter and expected to peak at Very Strong, seasonal outlooks suggest higher potential for erratic rainfall and lingering warmth over the next 1-3 months.

Generated by Gemini from climate data and web sources

At a Glance

Temperature – Average

Djibouti
Global
Land + Ocean
Sep
+2.8°C· 4th
32.9°C
+1.2°C· 2nd
16.3°C
Record
34.0°C (2023)
16.4°C (2023)
Jul–Sep
+3.3°C· 2nd
34.1°C
+1.1°C· 1st
16.7°C
Record
34.5°C (2023)
16.7°C (2026)
2025
+1.6°C· 3rd
29.1°C
+1.0°C· 3rd
15.0°C
Record
29.6°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 – Djibouti

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 Djibouti's climate

ENSO matters in Djibouti, most of all in January-March: the El Niño-La Niña cycle explains about 24% of the year-to-year swing in Djibouti's January-March temperatures, with El Niño years tending warmer and La Niña years cooler. That puts Djibouti 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

Djibouti's temperatures for January-March 1956 ran -0.6°C against the 1961-90 average - the cool January-March 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

Djibouti's temperatures for January-March 1974 ran -0.8°C against the 1961-90 average - the cool January-March 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

The strongest El Niño since 1950 on NOAA's Relative Oceanic Niño Index, which strips out the background warming of the tropical oceans before ranking events. On the older index that leaves that warming in, 2015-16 comes out on top instead.

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

Djibouti's temperatures for January-March 1989 ran -0.4°C against the 1961-90 average - the cool January-March 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 does not show in Djibouti's own record: 1992, the year after the June 1991 eruption, was an unremarkable year there, 31st-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

Djibouti's temperatures for January-March 1998 ran +1.4°C against the 1961-90 average - the warm January-March 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

1999-2001ENSO

The 1999-2001 La Niña

Djibouti's temperatures for January-March 2000 ran +0.4°C against the 1961-90 average - the opposite of the cool January-March 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

Djibouti's temperatures for January-March 2008 ran -0.5°C against the 1961-90 average - the cool January-March that La Niña usually brings here.

ONI -1.8°C · RONI -1.7°C

NOAA CPCENSO Tracker

2009-10ENSO

2009-10 El Niño

Djibouti's temperatures for January-March 2010 ran +0.6°C against the 1961-90 average - the warm January-March 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

Djibouti's own heatwave days - days in warm spells well above the local norm - rose from a 1961-90 average of 2.0 a year to 25.8 in 2016-25 - 13 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

2010-11Drought

Horn of Africa drought and famine, 2010-11

The October-December 2010 short rains failed across the Horn of Africa during La Niña and a negative Indian Ocean Dipole, and the 2011 long rains failed too - one of the region's worst droughts in decades. On 20 July 2011 the UN declared famine in parts of southern Somalia, and a later FSNAU / FEWS NET study estimated that about 258,000 people died in Somalia between October 2010 and April 2012, half of them children under five. On this site's rainfall record, Djibouti's October-December 2010 was the sixth-driest since 1950, 89% below its 1961-90 average.

Lott et al. (2013), NOAA Climate.gov, NOAA Climate.gov (2), UN press, FAO SomaliaIndian Ocean Dipole

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

Djibouti's temperatures for January-March 2016 ran +1.3°C against the 1961-90 average - the warm January-March 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. Djibouti tracks that closely - nine of its own eleven warmest fall in the same span, with only 1998 and 1990 outside. Its warmest year is 2024.

Learn more →

2019Flood

The Djibouti floods, 2019

Between 21 and 24 November 2019 almost 300 mm of rain fell on Djibouti city - more than three times its annual average, with two years' rain falling in a single day at the peak. The floods affected about 250,000 people, a quarter of the country's population, and around ten people were killed.

OCHA, ReliefWeb

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

Djibouti's temperatures for January-March 2021 ran +0.2°C against the 1961-90 average - the opposite of the cool January-March La Niña usually brings here.

ONI -1.1°C · RONI -1.5°C

WMO, WMO (2)ENSO Tracker

2023-24ENSO

2023-24 El Niño

Djibouti's temperatures for January-March 2024 ran +2.0°C against the 1961-90 average - the warm January-March 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 – Djibouti

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 – Djibouti

1940→20261961–1990 baselineColdest (1950)2016–2025 meanWarmest (2024)2026 so far
2026Sep
WetDryJanFebMarAprMayJunJulAugSepOctNovDec1891-19202016-25Wet Start−12 days1891-19202016-25Wet End+23 days25°30°35°
Temp
30.2°C
+2.4 vs base
Precipitation
123mm
-41 vs base
ENSO
—
RONI 3-mo mean
Playback
8×

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

Monthly Temperature – Djibouti

All years since 19502024 (Warmest)1950 (Coldest)2026 (Current Year)

Background lines: the last 40 years.

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

Records – Djibouti

Latest data Sep 2026
Warmest year
2024
29.7°C
Coldest year
1950
24.7°C
2026 so far
#2/87
30.2°C

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

Typical Climate – Djibouti

Köppen BWh · Arid

Djibouti has a arid climate (Köppen BWh: Hot desert), with both a warm/cold cycle and a wet/dry cycle through the year. June is typically the warmest month, averaging 34.0°C, while January is the coldest at 23.7°C. Annual precipitation averages around 216mm, concentrated mostly in the wet season.

Warmest month
Jun 34°C
Coldest month
Jan 24°C
Annual rainfall
216mm
Wettest month
Aug 35mm

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 BWh · Arid

Djibouti has both a clear warm/cold cycle (±4.6°C) and a wet/dry cycle (7× wet:dry ratio). Both sides of the annual rhythm are shown below.

Shifting summer
46 days Longer
Warm Season
1940–1969 Baseline: 14 Apr → 15 Oct · 185 days
2016–2025 Now: 21 Mar → 6 Nov · 231 days
−24d
+22d
J
F
M
A
M
J
J
A
S
O
N
D
Spr 24 days EarlierAut 22 days Later
Shifting wet season
34 days Longer
Wet Season
1891–1920 Baseline: 27 Aug → 12 Mar · 197 days
2016–2025 Now: 16 Aug → 4 Apr · 231 days
−12d
+23d
J
F
M
A
M
J
J
A
S
O
N
D
Onset 11 days EarlierEnd 23 days Later
+33.6% annual rain
baseline avgrecent avgClick a marker for each decade
Wet-season onset
27 Aug→16 Aug
12 days Earlier
When 25% of annual rain has fallen
Wet-season end
12 Mar→4 Apr
23 days Later
When 75% of annual rain has fallen
Peak-rain month
Mar→Aug
+5 month
Wet months: 5 → 7
1891–19202016–2025Wet-month threshold (13 mm)

Monthly precipitation climatology. A “wet month” exceeds the baseline monthly mean (dashed gold line). Biggest month-to-month shift: May (+18 mm, +325%).

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

Extreme Weather

Alerts & Disasters - Djibouti

Live GDACS alerts in Djibouti - 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

0

None since 2021

Moderate

0

Weather Disasters in 2025 - Latest Complete Year

Disasters

0

0.4 a year, 2016-2025

Deaths

0

2.1 a year, 2016-2025

Weather Disasters, 2016-2025

Most Frequent

Flood

2 of 4 disasters

Deadliest

Flood

19 of 21 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 - Djibouti

The natural climate patterns that measurably shape seasonal temperature or rainfall in Djibouti, 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)moderate 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 Jan-Mar temperature: El Niño tends to bring warmer conditions here, La Niña the reverse (about 24% of year-to-year variation).

ENSO Tracker
Indian Ocean Dipole (IOD)moderate link

ENSO's Indian Ocean partner - measured here beyond ENSO's own effect.

Now: positive · +0.88°C (BOM weekly DMI, week to 2026-10-18)

Strongest in Oct-Dec rainfall: a positive IOD tends to bring wetter conditions here, a negative IOD the reverse (about 19% of year-to-year variation).

Indian Ocean Dipole

Emissions & Energy

Explore

Explore Climate Data

Data Sources

Data Sources for Djibouti

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 Djibouti changing?

Djibouti 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 Djibouti?

Djibouti has a arid climate (Köppen BWh: Hot desert), with both a warm/cold cycle and a wet/dry cycle through the year. June is typically the warmest month, averaging 34.0°C, while January is the coldest at 23.7°C. Annual precipitation averages around 216mm, concentrated mostly in the wet season.

Which climate drivers affect the weather in Djibouti?

Measured from seasonal temperature and rainfall in Djibouti 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) - moderate, strongest in Jan-Mar temperature, which El Niño tends to make warmer here (La Niña the reverse), about 24% of year-to-year variation; the Indian Ocean Dipole (IOD) - moderate, strongest in Oct-Dec rainfall, which a positive IOD tends to make wetter here (a negative IOD the reverse), about 19% of year-to-year variation. Their current state is shown in the Climate Drivers section of this page.

What extreme weather affects Djibouti?

In 2025, the latest complete year, the international disaster database EM-DAT recorded 0 weather and climate disasters in Djibouti, against an average of 0.4 a year in 2016-2025, with 0 deaths. Over those ten years the most frequent type was flood (2 of 4) and the deadliest flood. GDACS, the UN and European Commission's disaster alert system, issued 0 Major (Red) and 0 Severe (Orange) alerts for Djibouti in the last 12 months. Live alerts are on this page and on the Extreme Weather tracker.

Where does the climate data for Djibouti come from?

Climate data for Djibouti 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 Djibouti climate data cover?

The Djibouti climate profile covers Djibouti City, Ali Sabieh, Dikhil, Tadjourah and surrounding areas. Temperature, rainfall and emissions data for Djibouti

How often is the Djibouti climate update refreshed?

The Djibouti 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 Djibouti 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 Djibouti 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 Djibouti experienced?

Major climate events in Djibouti include Horn of Africa drought and famine, 2010-11; The 1955-56 La Niña; The 1988-89 La Niña; 1997-98 El Niño; The 2007-08 La Niña; Global heatwave days sharply accelerate (2010); 2015-2025: the eleven warmest years on record; 2023-24 El Niño. The Climate History panel on this page lists 33 sourced events and pattern shifts relevant to Djibouti, the earliest from 1912 - 2 about Djibouti 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 Djibouti 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. 15 of the 33 entries here are written specifically about Djibouti, 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.