Hydrological cycle, temperature, and land surface-atmosphere interaction in the la Plata Basin during summer: Response to climate change

The austral summer response (2071-2100 with respect to 1981-2010) in terms of precipitation, temperature, and evapotranspiration was analyzed over South America, with emphasis on the La Plata Basin (LPB), using an ensemble of regional climate models. Seasonal mean pre - cipitation increased over the...

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Autores principales:	Menéndez, C.G., Zaninelli, P.G., Carril, A.F., Sánchez, E.
Formato:	JOUR
Materias:	Ensemble of regional climate models Evapotranspiration regimes Land-temperature coupling South America Temperature variability climate change climate modeling ensemble forecasting evapotranspiration hydrological cycle hydrological regime hydrological response hydrometeorology precipitation (climatology) regional climate seasonal variation summer Argentina La Plata Basin Rio de la Plata
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_0936577X_v68_n2-3_p231_Menendez
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

id	todo:paper_0936577X_v68_n2-3_p231_Menendez
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spelling	todo:paper_0936577X_v68_n2-3_p231_Menendez2023-10-03T15:48:41Z Hydrological cycle, temperature, and land surface-atmosphere interaction in the la Plata Basin during summer: Response to climate change Menéndez, C.G. Zaninelli, P.G. Carril, A.F. Sánchez, E. Ensemble of regional climate models Evapotranspiration regimes Land-temperature coupling South America Temperature variability climate change climate modeling ensemble forecasting evapotranspiration hydrological cycle hydrological regime hydrological response hydrometeorology precipitation (climatology) regional climate seasonal variation summer Argentina La Plata Basin Rio de la Plata The austral summer response (2071-2100 with respect to 1981-2010) in terms of precipitation, temperature, and evapotranspiration was analyzed over South America, with emphasis on the La Plata Basin (LPB), using an ensemble of regional climate models. Seasonal mean pre - cipitation increased over the southern LPB, consistent with CMIP3 and CMIP5 ensembles. However, the region of wetting (in the sense of precipitation minus evapotranspiration) over the LPB shifts to the north and northwest, compared to the region of increased precipitation. The LPB is characterized as the South American region with the largest gradient in temperature change (maximum warming north of the LPB and lowest temperature rise near the Rio de la Plata). The interannual variability of evapotranspiration has a geographic distribution similar to that of temperature variability, with a maximum in northern Argentina, suggesting that the 2 variables are interrelated. In turn, in the current climate, the southern LPB is a transition zone in which the evapotranspiration regime depends on the availability of soil water. The model ensemble also points to a similar geographical distribution of limitation regimes (energy- vs. soil moisture-limited evapotranspiration) for present-day and future conditions over South America. In particular, the evapotranspiration regime is projected to continue to be soil moisture-limited over the LPB. Nevertheless, the coupling between land and temperature decreases in areas with increasing soil water availability. In the southern LPB, interannual variability in temperature and evapotranspiration tend to decrease, while rainfall variability exhibits the opposite behavior. © Inter-Research 2016. Fil:Menéndez, C.G. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Zaninelli, P.G. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Carril, A.F. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_0936577X_v68_n2-3_p231_Menendez
institution	Universidad de Buenos Aires
institution_str	I-28
repository_str	R-134
collection	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic	Ensemble of regional climate models Evapotranspiration regimes Land-temperature coupling South America Temperature variability climate change climate modeling ensemble forecasting evapotranspiration hydrological cycle hydrological regime hydrological response hydrometeorology precipitation (climatology) regional climate seasonal variation summer Argentina La Plata Basin Rio de la Plata
spellingShingle	Ensemble of regional climate models Evapotranspiration regimes Land-temperature coupling South America Temperature variability climate change climate modeling ensemble forecasting evapotranspiration hydrological cycle hydrological regime hydrological response hydrometeorology precipitation (climatology) regional climate seasonal variation summer Argentina La Plata Basin Rio de la Plata Menéndez, C.G. Zaninelli, P.G. Carril, A.F. Sánchez, E. Hydrological cycle, temperature, and land surface-atmosphere interaction in the la Plata Basin during summer: Response to climate change
topic_facet	Ensemble of regional climate models Evapotranspiration regimes Land-temperature coupling South America Temperature variability climate change climate modeling ensemble forecasting evapotranspiration hydrological cycle hydrological regime hydrological response hydrometeorology precipitation (climatology) regional climate seasonal variation summer Argentina La Plata Basin Rio de la Plata
description	The austral summer response (2071-2100 with respect to 1981-2010) in terms of precipitation, temperature, and evapotranspiration was analyzed over South America, with emphasis on the La Plata Basin (LPB), using an ensemble of regional climate models. Seasonal mean pre - cipitation increased over the southern LPB, consistent with CMIP3 and CMIP5 ensembles. However, the region of wetting (in the sense of precipitation minus evapotranspiration) over the LPB shifts to the north and northwest, compared to the region of increased precipitation. The LPB is characterized as the South American region with the largest gradient in temperature change (maximum warming north of the LPB and lowest temperature rise near the Rio de la Plata). The interannual variability of evapotranspiration has a geographic distribution similar to that of temperature variability, with a maximum in northern Argentina, suggesting that the 2 variables are interrelated. In turn, in the current climate, the southern LPB is a transition zone in which the evapotranspiration regime depends on the availability of soil water. The model ensemble also points to a similar geographical distribution of limitation regimes (energy- vs. soil moisture-limited evapotranspiration) for present-day and future conditions over South America. In particular, the evapotranspiration regime is projected to continue to be soil moisture-limited over the LPB. Nevertheless, the coupling between land and temperature decreases in areas with increasing soil water availability. In the southern LPB, interannual variability in temperature and evapotranspiration tend to decrease, while rainfall variability exhibits the opposite behavior. © Inter-Research 2016.
format	JOUR
author	Menéndez, C.G. Zaninelli, P.G. Carril, A.F. Sánchez, E.
author_facet	Menéndez, C.G. Zaninelli, P.G. Carril, A.F. Sánchez, E.
author_sort	Menéndez, C.G.
title	Hydrological cycle, temperature, and land surface-atmosphere interaction in the la Plata Basin during summer: Response to climate change
title_short	Hydrological cycle, temperature, and land surface-atmosphere interaction in the la Plata Basin during summer: Response to climate change
title_full	Hydrological cycle, temperature, and land surface-atmosphere interaction in the la Plata Basin during summer: Response to climate change
title_fullStr	Hydrological cycle, temperature, and land surface-atmosphere interaction in the la Plata Basin during summer: Response to climate change
title_full_unstemmed	Hydrological cycle, temperature, and land surface-atmosphere interaction in the la Plata Basin during summer: Response to climate change
title_sort	hydrological cycle, temperature, and land surface-atmosphere interaction in the la plata basin during summer: response to climate change
url	http://hdl.handle.net/20.500.12110/paper_0936577X_v68_n2-3_p231_Menendez
work_keys_str_mv	AT menendezcg hydrologicalcycletemperatureandlandsurfaceatmosphereinteractioninthelaplatabasinduringsummerresponsetoclimatechange AT zaninellipg hydrologicalcycletemperatureandlandsurfaceatmosphereinteractioninthelaplatabasinduringsummerresponsetoclimatechange AT carrilaf hydrologicalcycletemperatureandlandsurfaceatmosphereinteractioninthelaplatabasinduringsummerresponsetoclimatechange AT sancheze hydrologicalcycletemperatureandlandsurfaceatmosphereinteractioninthelaplatabasinduringsummerresponsetoclimatechange
_version_	1782025645010714624

Hydrological cycle, temperature, and land surface-atmosphere interaction in the la Plata Basin during summer: Response to climate change

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