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southern-africa-climate-risk-report-final-.pdf
in these islands are greater than 1500mm per year (Figure 4). Observed trends in regional climate for Southern Africa Observational records show that Southern Africa’s average annual surface temperatures increased by between 1°C and 1.5°C from 1961 to 2015. Minimum temperatures have increased more
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southern-africa-climate-risk-report-final-pdf
in these islands are greater than 1500mm per year (Figure 4). Observed trends in regional climate for Southern Africa Observational records show that Southern Africa’s average annual surface temperatures increased by between 1°C and 1.5°C from 1961 to 2015. Minimum temperatures have increased more
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climate-risk-report-for-sea---v6-final-april-2026.pdf
as a result of human-induced climate change (Oliver et al., 2018). This marine heatwave persisted for 298 days, the longest on record for this region, with an average intensity of 2°C (Iskandar et al., 2021). Precipitation has generally increased by around 0.2- 0.5mm/day per decade, although this trend
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trd---climate-risk-report-for-csa---v4-final.pdf
to lack of reliable observation records (Fallah et al., 2023). Central Asian countries such as Kyrgyzstan and Tajikistan have very complex topography which requires high resolution climate data (~30km) for regional trend attribution studies (Fallah et 16 al., 2023). Central Asian trend attribution
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2024: record-breaking watershed year for global climate
2024 was the warmest year on record globally and the first year that was likely more than 1.5°C above pre-industrial levels: a stark reminder global temperatures are continuing to rise.
exceeded the previous warmest year – 2016 - by 0.17°C, making 2024 and 2023 the warmest and second-warmest years on record. A number of global climate centres will be releasing their 2024 average temperature figures today. The latest figures highlight how the world is getting closer to breaching
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IPCC expresses urgency of tackling climate change
Following two weeks of intense negotiations, the third report in the Intergovernmental Panel on Climate Change’s (IPCC) Sixth Assessment Report has been published today [Monday 4 April, 2022].
Known as the Working Group III report, the document provides an up-to-date assessment of the scientific knowledge on climate change mitigation, assessing methods for reducing greenhouse gas emissions, and removing greenhouse gases from the atmosphere. Professor Jason Lowe OBE is the Head of Climate
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Global impacts of climate change - observed trends
These maps show the observed regional trends in 6 types of climate extremes and impacts, with examples of impactful extreme weather events attributable partly or wholly to anthropogenic climate change.
Regions around the world are experiencing multiple increasing climate extremes and impacts. The maps show regions where recent decades have seen increases in extreme heat, heavy rainfall, agricultural drought, and the length of the fire weather season, as well as changes in river flows, and glacier
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02427 South Asia climate infographic-v4
Central and South Asia Climate Risk Report – South Asia HEADLINE CLIMATE STATEMENTS AFGHANISTAN IRAN CHINA PAKISTAN NEPAL BHUTAN INDIA BANGLADESH Most of South Asia has warmed by around 0.1 to 0.2°C per decade during 1980 to 2015, with Pakistan and Afghanistan warming 0.4 to 0.5°C per decade
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climate-outlook-user-guide---april-2025docx
Climate Outlook User Guide The aim of the Met Office’s Climate Outlook product is to provide seasonal information, reviewing the last three months and looking forward 3-6 months, so that readers are informed of the seasonal variability affecting various countries. Multiple climate hazards
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HadGEM1: Met Office climate prediction model
HadGEM1 is the first in a new generation of coupled climate models incorporating a non-hydrostatic, fully compressible, deep atmosphere formulation with a semi-implicit semi-Lagrangian time integration scheme.
Note that the most recent HadGEM model is the HadGEM3 HadGEM1 stands for the Hadley Centre Global Environment Model version 1. It was developed in 2006 and used in the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. The atmospheric component has 38 levels extending