Volume 38, Issue 14 p. 5095-5106
RESEARCH ARTICLE

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

Assaf Hochman,

Corresponding Author

Assaf Hochman

Department of Geosciences, School of Geosciences, Tel Aviv University, Tel-Aviv, Israel

Porter School of Environmental Studies, School of Geosciences, Tel-Aviv University, Tel-Aviv, Israel

Department of Geography and the Human Environment, School of Geosciences, Tel-Aviv University, Tel-Aviv, Israel

Correspondence

Assaf Hochman, Department of Geosciences, School of Geosciences, Tel-Aviv University, Tel-Aviv 69978, Israel.

Email: assafhochman@post.tau.ac.il; assafhochman@yahoo.com

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Paola Mercogliano,

Paola Mercogliano

CMCC Euro-Mediterranean Center on Climate Change, Capua, Italy

CIRA Centro Italiano Ricerche Aerospaziali, Capua, Italy

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Pinhas Alpert,

Pinhas Alpert

Department of Geosciences, School of Geosciences, Tel Aviv University, Tel-Aviv, Israel

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Hadas Saaroni,

Hadas Saaroni

Department of Geography and the Human Environment, School of Geosciences, Tel-Aviv University, Tel-Aviv, Israel

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Edoardo Bucchignani,

Edoardo Bucchignani

CMCC Euro-Mediterranean Center on Climate Change, Capua, Italy

CIRA Centro Italiano Ricerche Aerospaziali, Capua, Italy

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First published: 14 August 2018
Citations: 18
Funding information German Helmholtz Association; Ministry of Science and Technology (MOST); Italian Ministry of the Environment, Land and Sea; Italian Ministry of Education

Abstract

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 ~2.5 °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 ~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.