Climate change indicators reached record levels in 2023: WMO

Greenhouse gases

Observed concentrations of the three main greenhouse gases – carbon dioxide, methane, and nitrous oxide – reached record levels in 2022. Real-time data from specific locations show a continued increase in 2023.

CO2 levels are 50 % higher than the pre-industrial era, trapping heat in the atmosphere. The long lifetime of CO2 means that temperatures will continue to rise for many years to come.

Temperature

The global mean near-surface temperature in 2023 was 1.45 ± 0.12 °C above the pre-industrial 1850–1900 average. 2023 was the warmest year in the 174-year observational record. This shattered the record of the previous warmest years, 2016 at 1.29 ± 0.12 °C above the 1850–1900 average and 2020 at 1.27±0.13 °C.

The ten-year average 2014–2023 global temperature is 1.20±0.12°C above the 1850–1900 average. 
Globally, every month from June to December was record warm for the respective month. September 2023 was particularly noteworthy, surpassing the previous global record for September by a wide margin (0.46 to 0.54 °C).

The long-term increase in global temperature is due to increased concentrations of greenhouse gases in the atmosphere. The shift from La Niña to El Niño conditions in the middle of 2023 contributed to the rapid rise in temperature from 2022 to 2023.

Global average sea-surface temperatures (SSTs) were at a record high from April onwards, with the records  in July, August and September broken by a particularly wide margin. Exceptional warmth was recorded in the eastern North Atlantic, the Gulf of Mexico and the Caribbean, the North Pacific and large areas of the Southern Ocean, with widespread marine heatwaves.

Some areas of unusual warming such as the Northeast Atlantic do not correspond to typical patterns of warming associated with El Niño, which was visibly present in the Tropical Pacific.

Ocean heat

Global map showing the highest Marine Heatwave category in each pixel over 2023 (reference period 1982–2011).

Ocean heat content reached its highest level in 2023, according to a consolidated analysis of data. Warming rates show a particularly strong increase in the past two decades.

It is expected that warming will continue – a change which is irreversible on scales of hundreds to thousands of years.

More frequent and intense marine heatwaves have profound negative repercussions for marine ecosystems and coral reefs.

The global ocean experienced an average daily marine heatwave coverage of 32%, well above the previous record of 23% in 2016. At the end of 2023, most of the global ocean between 20° S and 20° N had been in heatwave conditions since early November.  

Of particular note were the widespread marine heatwaves in the North Atlantic which began in the Northern Hemisphere spring, peaked in extent in September and persisted through to the end of the year. The end of 2023 saw a broad band of severe and extreme marine heatwave across the North Atlantic, with temperatures 3 °C above average.

The Mediterranean Sea experienced near complete coverage of strong and severe marine heatwaves for the twelfth consecutive year.

Ocean acidification has increased as a result of absorbing carbon dioxide.

Sea level rise

In 2023, global mean sea level reached a record high in the satellite record (since 1993), reflecting continued ocean warming (thermal expansion) as well as the melting of glaciers and ice sheets.

The rate of global mean sea level rise in the past ten years (2014–2023) is more than twice the rate of sea level rise in the first decade of the satellite record (1993–2002).

Cryosphere

Daily Antarctic sea-ice extent from January through December, showing 2023 (red) conditions against the 1991–2020 climate normal (dark blue) and the record highest and lowest extents for each day (mid blue). Individual years are shown in light blue.

U.S. National Snow and Ice Data Center.

Antarctic sea-ice extent reached an absolute record low for the satellite era (since 1979) in February 2023 and remained at record low for the time of year from June till early November. The annual maximum in September was 16.96 million km2, roughly 1.5 million km2 below the 1991–2020 average and 1 million km2 below the previous record low maximum.

Arctic sea-ice extent remained well below normal, with the annual maximum and minimum sea ice extents being the fifth and sixth lowest on record respectively.

Ice sheets: There are two principal ice sheets, the Greenland Ice Sheet and the Antarctic ice Sheet. Combining the two ice sheets, the seven highest melt years on record are all since 2010, and average rates of mass loss increased from 105 Gigatonnes per year  from 1992–1996 to 372 Gigatonnes per year from 2016–2020. This is equivalent to about 1 mm per year of global sea level rise attributed to the ice sheets in the latter period.

The Greenland Ice Sheet continued to lose mass in the hydrological year 2022–2023 It was the warmest summer on record at Greenland’s Summit station, 1.0 °C warmer than the previous record. Satellite melt-extent data indicate that the ice sheet had the third highest cumulative melt-day area on record (1978–2023), after the extreme melt season of 2012 and 2010.

Glaciers: Preliminary data for the hydrological year 2022-2023 indicate that the global set of reference glaciers suffered the largest loss of ice on record (1950-2023), driven by extremely negative mass balance in both western North America and Europe.

Glaciers in the European Alps experienced an extreme melt season. In Switzerland, glaciers have lost around 10% of their remaining volume in the past two years. Western North America suffered record glacier mass loss in 2023 – at a rate which was five times higher than rates measured for the period 2000-2019. Glaciers in western North America have lost an estimated 9% of their 2020 volume over the period 2020-2023.

Extreme weather and climate events

Extreme weather and climate events had major socio-economic impacts on all inhabited continents. These included major floods, tropical cyclones, extreme heat and drought, and associated wildfires.

Flooding linked to extreme rainfall from Mediterranean Cyclone Daniel affected Greece, Bulgaria, Türkiye, and Libya with particularly heavy loss of life in Libya in September.

Tropical Cyclone Freddy in February and March was one of the world’s longest-lived tropical cyclones with major impacts on Madagascar, Mozambique and Malawi.

Tropical Cyclone Mocha, in May, was one of the most intense cyclones ever observed in the Bay of Bengal and triggered 1.7 million displacements across the sub-region from Sri Lanka to Myanmar and through India and Bangladesh, and worsened acute food insecurity.

Hurricane Otis intensified to a maximum Category 5 system in a matter of hours – one of the most rapid intensification rates in the satellite era. It hit the Mexican coastal resort of Acapulco on 24 October, causing economic losses estimated at around US$15 billion, and killing at least 47 people.

Extreme heat affected many parts of the world. Some of the most significant were in southern Europe and North Africa, especially in the second half of July. Temperatures in Italy reached 48.2 °C, and record-high temperatures were reported in Tunis (Tunisia) 49.0 °C, Agadir (Morocco) 50.4 °C and Algiers (Algeria) 49.2 °C.

Canada’s wildfire season was the worst on record. The total area burned nationally for the year was 14.9 million hectares, more than seven times the long-term average. The fires also led to severe smoke pollution, particularly in the heavily populated areas of eastern Canada and the north-eastern United States. The deadliest single wildfire of the year was in Hawaii, with at least 100 deaths reported – the deadliest wildfire in the USA for more than 100 years – and estimated economic losses of US$5.6 billion.

The Greater Horn of Africa region, which had been experiencing long-term drought, suffered substantial flooding in 2023, particularly later in the year. The flooding displaced 1.8 million people across Ethiopia, Burundi, South Sudan, Tanzania, Uganda, Somalia and Kenya in addition to the 3 million people displaced internally or across borders by the five consecutive seasons of drought in Ethiopia, Kenya, Djibouti, and Somalia.

Long-term drought persisted in north-western Africa and parts of the Iberian Peninsula, as well as parts of central and southwest Asia. It intensified in many parts of Central America and South America. In northern Argentina and Uruguay, rainfall from January to August was 20 to 50% below average, leading to crop losses and low water storage levels.

Socioeconomic impacts

Global prevalence of undernourishment (as a%) and number of undernourished (in millions) since 2005. The entire series was updated to reflect new information released since the publication of The State of Food Security and Nutrition in the World 2023. NOTES: * Projections based on nowcasts for 2022 are illustrated by dotted lines. Bars show lower and upper bounds of the estimated range. SOURCE: FAO. 2023. FAOSTAT: Suite of Food Security Indicators. In: FAO. [Cited 12 July 2023]. www.fao.org/faostat/en/#data/FS

Source: The State of Food Security and Nutrition in the World 2023, FAO. 2023

Weather and climate hazards exacerbated challenges with food security, population displacements and impacts on vulnerable populations. They continued to trigger new, prolonged, and secondary displacement and increased the vulnerability of many who were already uprooted by complex multi-causal situations of conflict and violence.

One of the essential components for reducing the impact of disasters is to have effective multi-hazard early warning systems. The Early Warnings for All initiative seeks to ensure that everyone is protected by early warning systems by the end of 2027. Development and implementation of local disaster risk reduction strategies have increased since the adoption of the Sendai Framework for Disaster Risk Reduction.

The report cites figures that the number of people who are acutely food insecure worldwide has more than doubled, from 149 million people before the COVID-19 pandemic to 333 million people in 2023 (in 78 monitored countries by the World Food Programme). WFP Global hunger levels remained unchanged from 2021 to 2022. However, these are still far above pre-COVID 19 pandemic levels: in 2022, 9.2% of the global population (735.1 million people) were undernourished. Protracted conflicts, economic downturns, and high food prices, further exacerbated by high costs of agricultural inputs driven by ongoing and widespread conflict around the world, are at the root of high global food insecurity levels. This is aggravated by the effects of climate and weather extremes. In southern Africa, for example, the passage of Cyclone Freddy in February 2023 affected Madagascar, Mozambique, southern Malawi, and Zimbabwe. Flooding submerged extensive agricultural areas and inflicted severe damage on crops and the economy.

Renewable energy generation, primarily driven by the dynamic forces of solar radiation, wind and the water cycle, has surged to the forefront of climate action for its potential to achieve decarbonization targets.

Worldwide, a substantial energy transition is already underway. In 2023, renewable capacity additions increased by almost 50% from 2022, for a total of 510 gigawatts (GW). Such growth marks the highest rate observed in the past two decades and indicates, demonstrates the potential to achieve the clean energy goal set at COP28 to triple renewable energy capacity globally to reach 11 000 GW by 2030.

Climate Financing

In 2021/2022, global climate-related finance flows reached almost USD 1.3 trillion, nearly doubling compared to 2019/2020 levels. Even so, tracked climate finance flows represent only approximately 1% of global GDP, according to the Climate Policy Initiative.

There is a large financing gap. In an average scenario, for a 1.5°C pathway, annual climate finance investments need to grow by more than six times, reaching almost USD 9 trillion by 2030 and a further USD 10 trillion through to 2050.  

The cost of inaction is even higher. Aggregating over the period 2025-2100, the total cost of inaction is estimated at USD 1,266 trillion; that is, the difference in losses under a business-as-usual scenario and those incurred within a 1.5°C pathway. This figure is, however, likely to be a dramatic underestimate.

Adaptation finance continues to be insufficient. Though adaptation finance reached an all-time high of USD 63 billion in 2021/2022, the global adaptation financing gap is widening, falling well short of the estimated USD 212 billion per year needed up to 2030 in developing countries alone.