Αποτελέσματα Αναζήτησης
This page presents high-level information for Iraq's climate zones and its seasonal cycle for mean temperature and precipitation for the latest climatology, 1991-2020.
- Climate Projections
This page presents Iraq's projected climate. The Mean...
- Sea Level Rise
The systematic warming of the planet is directly causing...
- Current Climate
This page presents Iraq's climate context for the current...
- Vulnerability
Changes in both the climate system and socioeconomic...
- Climate Change Overview
The Earth’s climate is changing and the global climate is...
- Climate Projections
An interactive visual window into our planet's changing climate, based on the most recent measurements and climate model predictions (read the research)
Iraq Climatic Classifications. Summary: Most regions (11) in Iraq lie in the Subtropical desert climate zone (Köppen: Bwh). The mean average of annual temperatures range from a high of 30.19°C (86.34°F) in Basra to a low of 20.06°C (68.11°F) in Dohuk.
This page presents Iraq's climate context for the current climatology, 1991-2020, derived from observed, historical data. Information should be used to build a strong understanding of current climate conditions in order to appreciate future climate scenarios and projected change.
UNEP IRAQ Climate GIS Data Portal. This GIS Portal has been produced in tandem with Climate Risk Assessment for Iraq report for the purpose of supporting UNEP contribute to the delivery of climate change adaptation in the Asian region through the Green Climate Fund funded National Adaptation Plan (NAP) for Iraq project.
In Iraq, the climate is desert in the center and the south, with mild winters and extremely hot summers, and it's semi-desert in the north, with relatively cold winters. In the northern mountains, the climate is cold and rainy (or snowy) in winter and hot and sunny in summer, but with cooler nights due to the high altitude.
Iraq has a Mediterranean climate, characterized by boreal winter rainfall and hot, dry summers. The climate variation across the country is influenced by latitude and the high mountains in the north. These high mountain areas are characterized by higher rainfall (400–1,000mm per year) than 25mm per year in some areas).
