Interdecadal Changes in Ocean Teleconnections with the Sahel Implications in Rainfall Predictability /

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 rain...

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Κύριος συγγραφέας: Suárez Moreno, Roberto (Συγγραφέας, http://id.loc.gov/vocabulary/relators/aut)
Συγγραφή απο Οργανισμό/Αρχή: SpringerLink (Online service)
Μορφή: Ηλεκτρονική πηγή Ηλ. βιβλίο
Γλώσσα:English
Έκδοση: Cham : Springer International Publishing : Imprint: Springer, 2019.
Έκδοση:1st ed. 2019.
Σειρά:Springer Theses, Recognizing Outstanding Ph.D. Research,
Θέματα:
Διαθέσιμο Online:Full Text via HEAL-Link
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245 1 0 |a Interdecadal Changes in Ocean Teleconnections with the Sahel  |h [electronic resource] :  |b Implications in Rainfall Predictability /  |c by Roberto Suárez Moreno. 
250 |a 1st ed. 2019. 
264 1 |a Cham :  |b Springer International Publishing :  |b Imprint: Springer,  |c 2019. 
300 |a XXIII, 185 p. 73 illus., 70 illus. in color.  |b online resource. 
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490 1 |a Springer Theses, Recognizing Outstanding Ph.D. Research,  |x 2190-5053 
505 0 |a Preface -- Chapter 1: Motivation -- Chapter 2: State-of-the-Art -- Chapter 3: Objectives -- Chapter 4: Physical Background -- Chapter 5: Data -- Chapter 6: Methodology -- Chapter 7: A Statistical Model based on Non-stationary Predictors -- Chapter 8: Interdecadal changes in the SST-driven teleconnections with the Sahel -- Chapter 9: Modulation of the non-stationary Mediterranean-Sahel teleconnection -- Chapter 10: Concluding Remarks -- Glossary -- References. 
520 |a 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 analyzes 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. 
650 0 |a Atmospheric sciences. 
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