4.6 Article

High-resolution projection of climate change and extremity over Israel using COSMO-CLM

Journal

INTERNATIONAL JOURNAL OF CLIMATOLOGY
Volume 38, Issue 14, Pages 5095-5106

Publisher

WILEY
DOI: 10.1002/joc.5714

Keywords

COSMO-CLM; downscaling; eastern Mediterranean; ETCCDI; extreme precipitation; extreme temperature; Israel; RCM

Funding

  1. Italian Ministry of Education
  2. Italian Ministry of the Environment, Land and Sea
  3. Ministry of Science and Technology (MOST) of the state of Israel
  4. Tel-Aviv University (TAU)
  5. Mintz foundation
  6. Porter School of Environmental Studies at TAU
  7. German Helmholtz Association within the Virtual Institute DESERVE (Dead Sea Research Venue) [VH-VI-527]

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High-resolution climate projections over Israel (about 8 km) have been obtained with the regional model COSMO-CLM, nested into the CORDEX-MENA simulations at 25 km resolution. This simulation provides high-resolution spatial variability of total precipitation and precipitation intensity. Projections are presented not only in terms of average properties, but also using a subset of extreme temperature and precipitation indices from the standard Expert Team on Climate Change Detection and Indices (ETCCDI) for the period 2041-2070 with respect to 1981-2010 (RCP4.5). A general increase in seasonal mean temperature is projected throughout the domain with peaks of similar to 2.5 degrees C, especially in winter and autumn. Extreme temperature indices show increases, larger in the minimum than in the maximum temperatures. Regarding total seasonal precipitation, decreases were found in the north and central Mediterranean climate parts of Israel, with reductions reaching similar to 40%, and increases of the same percentage in the most southern arid parts during winter and spring. An increase in precipitation intensity is shown mostly for the southern arid part of the region, with some indications of extremity also in the north. This spatial pattern probably results from a decrease in cyclones' occurrences, which mainly influences the northern and central parts of Israel, and an increase in convective activity in the south. The outcome of this study can serve as a basis for priority setting and policy formulation towards better climate adaptation.

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