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Titlebook: Interdecadal Changes in Ocean Teleconnections with the Sahel; Implications in Rain Roberto Suárez Moreno Book 2019 Springer Nature Switzerl

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書(shū)目名稱(chēng)Interdecadal Changes in Ocean Teleconnections with the Sahel
副標(biāo)題Implications in Rain
編輯Roberto Suárez Moreno
視頻videohttp://file.papertrans.cn/471/470750/470750.mp4
概述Nominated as an outstanding PhD thesis by the University Complutense of Madrid, Madrid, Spain.Demonstrates for the first time the unstable behavior of the sea surface temperature-forced response of mo
叢書(shū)名稱(chēng)Springer Theses
圖書(shū)封面Titlebook: Interdecadal Changes in Ocean Teleconnections with the Sahel; Implications in Rain Roberto Suárez Moreno Book 2019 Springer Nature Switzerl
描述In tropical latitudes, monsoons trigger regimes of strong seasonal rainfall over the continents. Over the West African region, the rainfall has shown a strong variability from interannual to decadal time scales. The atmospheric response to global sea surface temperatures is the leading cause of rainfall variability in the West African Sahel. This thesis explores changes in the leading ocean forcing of Sahelian rainfall interannual variability. It anaylzes the dynamical mechanisms at work to explain the non-stationary sea surface temperature-forced response of anomalous rainfall. The underlying multidecadal sea surface temperature background is raised as a key factor that favors some interannual teleconnections and inhibits others. Results of this thesis are relevant for improving the seasonal predictability of summer rainfall in the Sahel.
出版日期Book 2019
關(guān)鍵詞West African Monsoon; Sahelian rainfall; climate variability; interannual variability; multidecadal vari
版次1
doihttps://doi.org/10.1007/978-3-319-99450-5
isbn_ebook978-3-319-99450-5Series ISSN 2190-5053 Series E-ISSN 2190-5061
issn_series 2190-5053
copyrightSpringer Nature Switzerland AG 2019
The information of publication is updating

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https://doi.org/10.1007/978-3-319-99450-5West African Monsoon; Sahelian rainfall; climate variability; interannual variability; multidecadal vari
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State of the Art, than the one that is absorbed (Fig. 2.1). To compensate this imbalance, atmospheric and oceanic transport processes distribute the energy around the globe. Atmospheric winds and ocean currents accomplish this transport. From a dynamical point of view, the oceans and the atmosphere must be considered together as components of the climate system.
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