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Titlebook: Mediterranean Climate; Variability and Tren Hans-Jürgen Bolle Book 2003 Springer-Verlag Berlin Heidelberg 2003 Aerosol.Atmospheric circulat

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發(fā)表于 2025-3-21 19:03:49 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Mediterranean Climate
副標(biāo)題Variability and Tren
編輯Hans-Jürgen Bolle
視頻videohttp://file.papertrans.cn/630/629824/629824.mp4
概述For the first time results inferred by a number of experts from empirical data with various methods face each other and are collated to a large overview of the climate variability in the Mediterranean
叢書名稱Regional Climate Studies
圖書封面Titlebook: Mediterranean Climate; Variability and Tren Hans-Jürgen Bolle Book 2003 Springer-Verlag Berlin Heidelberg 2003 Aerosol.Atmospheric circulat
描述Mohamed Larbi Selassi Deputy Director of the National Meteorology, Morocco Welcome address (translated from French) WMO, WCRP, Medias-France and scientific institutions representatives, ladies and gentlemen, to thank WMO and MEDIAS-France, who have honoured us by I want first organizing the two workshops, climate indices in Africa and data assessment for global change research in the Mediterranean region, in Casablanca and I welcome all of you here in Morocco. It is with great pleasure that I open these two workshops on behalf of myself and on behalf of the Direction of the Meteorologie N ationale of Morocco. Climate change is becoming the focus of the international community because of its global scale and unpredictable effects, the numerous impacts it causes, its global feature and the complexity of the solutions that can mitigate its impacts. Global warming and the greenhouse effect became a subject of study at the international level since the United Nations Conference on the human environment that was held in Stockholm in 1972. The research and coordination efforts that have been made in this area have led to an "International Scientific consensus". High level meetings like th
出版日期Book 2003
關(guān)鍵詞Aerosol; Atmospheric circulation; Contamination; Precipitation; Scale; biosphere; climate change; ecology; h
版次1
doihttps://doi.org/10.1007/978-3-642-55657-9
isbn_softcover978-3-642-62862-7
isbn_ebook978-3-642-55657-9Series ISSN 1862-0248 Series E-ISSN 1865-505X
issn_series 1862-0248
copyrightSpringer-Verlag Berlin Heidelberg 2003
The information of publication is updating

書目名稱Mediterranean Climate影響因子(影響力)




書目名稱Mediterranean Climate影響因子(影響力)學(xué)科排名




書目名稱Mediterranean Climate網(wǎng)絡(luò)公開度




書目名稱Mediterranean Climate網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Mediterranean Climate被引頻次




書目名稱Mediterranean Climate被引頻次學(xué)科排名




書目名稱Mediterranean Climate年度引用




書目名稱Mediterranean Climate年度引用學(xué)科排名




書目名稱Mediterranean Climate讀者反饋




書目名稱Mediterranean Climate讀者反饋學(xué)科排名




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P. Maheras,C. Anagnostopoulou. Im allgemeinen dynamischen Fall kann sie sich aber auch mit der Zeit ?ndern. Somit sind die V.erschiebungskomponenten ξ, η und ζ im allgemeinen Fall Funktionen der Koordinaten und der Zeit: . = .(.), . = .(.), . = (.).
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Climate, Climate Variability, and Impacts in the Mediterranean Area: An Overviewtugal had great damage due to flooding because the rain was much above normal. In Valladolid it rained 106.8 mm which is the highest monthly total since 130 years. Segovia had the highest number of rainy days during the last century. Three severe tornados damaged Alicante, Murcia, and Granada. Up to
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Circulation Types and Their Influence on the Interannual Variability and Precipitation Changes in Grtation amounts. On the other hand the four more “rainy” circulation types, namely the C, C., C. and C. together represent 37.8% of all the rainy period days and account more than 72% of the observed daily precipitation. The results obtained accentuate the existence of the strong links between the in
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Temperature and Precipitation Variability and Trends in Northern Spain in the Context of the Iberianis of the principal components series using moving average and the Mann-Kendall test, show significant long term decreases in precipitation for Mediterranean region and Interior (at least in some seasons) and an increase of the precipitation for the Northern coastal region. The changes found have be
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