The marine climate over the Mediterranean Sea has been examined for the winter and summer seasons over the period 1946-1987. Little change was found in the winter over this period, apart from some evidence of a decline in the strength of the surface circulation. However, the summer months have seen a general rise in atmospheric pressure over the basin, with strengthening north- westerly winds in the eastern Mediterranean. Changes in the eastern and western basin are frequently out-of-phase because different processes tend to affect the climates of the two basins. These changes have been validated by analysis of the climate at land-based stations around the periphery of the Mediterranean. Combining the marine and terrestrial analyses shows possible links between climate in the eastern Mediterranean, changes in the intensity of the South Asian Monsoon (via reorientation of the summer-time trough over the Middle East), and climatic change over sub-Saharan Africa.
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Mie Univ, Grad Sch Bioresourres, 1577 Kurimamachiya Cho, Tsu, Mie 5148507, Japan
Univ Tokyo, Res Ctr Adv Sci & Technol, Tokyo, JapanMie Univ, Grad Sch Bioresourres, 1577 Kurimamachiya Cho, Tsu, Mie 5148507, Japan
Nishii, Kazuaki
Taguchi, Bunmei
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Univ Tokyo, Res Ctr Adv Sci & Technol, Tokyo, Japan
Univ Toyama, Fac Sustainable Design, Toyama, JapanMie Univ, Grad Sch Bioresourres, 1577 Kurimamachiya Cho, Tsu, Mie 5148507, Japan
机构:
Department of Meteorology and Hydrology, Faculty of Geography and Environmental Sciences al-Faraby Kazakh National Uni- versity, Almaty, KazakhstanDepartment of Meteorology and Hydrology, Faculty of Geography and Environmental Sciences al-Faraby Kazakh National Uni- versity, Almaty, Kazakhstan
Vitaly Salnikov
Galina Turulina
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Department of Meteorology and Hydrology, Faculty of Geography and Environmental Sciences al-Faraby Kazakh National Uni- versity, Almaty, KazakhstanDepartment of Meteorology and Hydrology, Faculty of Geography and Environmental Sciences al-Faraby Kazakh National Uni- versity, Almaty, Kazakhstan
Galina Turulina
Svetlana Polyakova
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Department of Meteorology and Hydrology, Faculty of Geography and Environmental Sciences al-Faraby Kazakh National Uni- versity, Almaty, KazakhstanDepartment of Meteorology and Hydrology, Faculty of Geography and Environmental Sciences al-Faraby Kazakh National Uni- versity, Almaty, Kazakhstan
Svetlana Polyakova
Marat Moldahmetov
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Department of Meteorology and Hydrology, Faculty of Geography and Environmental Sciences al-Faraby Kazakh National Uni- versity, Almaty, KazakhstanDepartment of Meteorology and Hydrology, Faculty of Geography and Environmental Sciences al-Faraby Kazakh National Uni- versity, Almaty, Kazakhstan
Marat Moldahmetov
Lyazzat Mahmudova
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Department of Meteorology and Hydrology, Faculty of Geography and Environmental Sciences al-Faraby Kazakh National Uni- versity, Almaty, KazakhstanDepartment of Meteorology and Hydrology, Faculty of Geography and Environmental Sciences al-Faraby Kazakh National Uni- versity, Almaty, Kazakhstan
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Colorado State Univ, Dept Atmospher Sci, Ft Collins, CO 80521 USA
Ludwig Maximilians Univ Munchen, Meteorol Inst, Munich, GermanyColorado State Univ, Dept Atmospher Sci, Ft Collins, CO 80521 USA
Davis, Luke L. B.
Thompson, David W. J.
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Colorado State Univ, Dept Atmospher Sci, Ft Collins, CO 80521 USA
Ludwig Maximilians Univ Munchen, Meteorol Inst, Munich, GermanyColorado State Univ, Dept Atmospher Sci, Ft Collins, CO 80521 USA