CMIP5 Simulations of low-level tropospheric temperature and moisture over the tropical Americas

Global warming has been linked to systematic changes in North and South America's climates and may severely impact the North American monsoon system (NAMS) and South American monsoon system (SAMS). This study examines interannual-to-decadal variations and changes in the low-troposphere (850 hPa) tem...

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Autores principales: Carvalho, Leila M. V., Jones, C., Posadas, A., Quiróz, R., Bookhagen, B., Liebmann, B.
Formato: Journal Article
Lenguaje:Inglés
Publicado: American Meteorological Society 2013
Materias:
Acceso en línea:https://hdl.handle.net/10568/52074
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author Carvalho, Leila M. V.
Jones, C.
Posadas, A.
Quiróz, R.
Bookhagen, B.
Liebmann, B.
author_browse Bookhagen, B.
Carvalho, Leila M. V.
Jones, C.
Liebmann, B.
Posadas, A.
Quiróz, R.
author_facet Carvalho, Leila M. V.
Jones, C.
Posadas, A.
Quiróz, R.
Bookhagen, B.
Liebmann, B.
author_sort Carvalho, Leila M. V.
collection Repository of Agricultural Research Outputs (CGSpace)
description Global warming has been linked to systematic changes in North and South America's climates and may severely impact the North American monsoon system (NAMS) and South American monsoon system (SAMS). This study examines interannual-to-decadal variations and changes in the low-troposphere (850 hPa) temperature (T850) and specific humidity (Q850) and relationships with daily precipitation over the tropical Americas using the NCEP–NCAR reanalysis, the Climate Forecast System Reanalysis (CFSR), and phase 5 of the Coupled Model Intercomparison Project (CMIP5) simulations for two scenarios: “historic” and high-emission representative concentration pathway 8.5 (RCP8.5). Trends in the magnitude and area of the 85th percentiles were distinctly examined over North America (NA) and South America (SA) during the peak of the respective monsoon season. The historic simulations (1951–2005) and the two reanalyses agree well and indicate that significant warming has occurred over tropical SA with a remarkable increase in the area and magnitude of the 85th percentile in the last decade (1996–2005). The RCP8.5 CMIP5 ensemble mean projects an increase in the T850 85th percentile of about 2.5°C (2.8°C) by 2050 and 4.8°C (5.5°C) over SA (NA) by 2095 relative to 1955. The area of SA (NA) with T850 ≥ the 85th percentile is projected to increase from ~10% (15%) in 1955 to ~58% (~33%) by 2050 and ~80% (~50%) by 2095. The respective increase in the 85th percentile of Q850 is about 3 g kg−1 over SAMS and NAMS by 2095. CMIP5 models project variable changes in daily precipitation over the tropical Americas. The most consistent is increased rainfall in the intertropical convergence zone in December–February (DJF) and June–August (JJA) and decreased precipitation over NAMS in JJA.
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spelling CGSpace520742025-11-13T10:39:09Z CMIP5 Simulations of low-level tropospheric temperature and moisture over the tropical Americas Carvalho, Leila M. V. Jones, C. Posadas, A. Quiróz, R. Bookhagen, B. Liebmann, B. climate agriculture monsoon climate troposphere models Global warming has been linked to systematic changes in North and South America's climates and may severely impact the North American monsoon system (NAMS) and South American monsoon system (SAMS). This study examines interannual-to-decadal variations and changes in the low-troposphere (850 hPa) temperature (T850) and specific humidity (Q850) and relationships with daily precipitation over the tropical Americas using the NCEP–NCAR reanalysis, the Climate Forecast System Reanalysis (CFSR), and phase 5 of the Coupled Model Intercomparison Project (CMIP5) simulations for two scenarios: “historic” and high-emission representative concentration pathway 8.5 (RCP8.5). Trends in the magnitude and area of the 85th percentiles were distinctly examined over North America (NA) and South America (SA) during the peak of the respective monsoon season. The historic simulations (1951–2005) and the two reanalyses agree well and indicate that significant warming has occurred over tropical SA with a remarkable increase in the area and magnitude of the 85th percentile in the last decade (1996–2005). The RCP8.5 CMIP5 ensemble mean projects an increase in the T850 85th percentile of about 2.5°C (2.8°C) by 2050 and 4.8°C (5.5°C) over SA (NA) by 2095 relative to 1955. The area of SA (NA) with T850 ≥ the 85th percentile is projected to increase from ~10% (15%) in 1955 to ~58% (~33%) by 2050 and ~80% (~50%) by 2095. The respective increase in the 85th percentile of Q850 is about 3 g kg−1 over SAMS and NAMS by 2095. CMIP5 models project variable changes in daily precipitation over the tropical Americas. The most consistent is increased rainfall in the intertropical convergence zone in December–February (DJF) and June–August (JJA) and decreased precipitation over NAMS in JJA. 2013-09-01 2014-12-16T06:37:30Z 2014-12-16T06:37:30Z Journal Article https://hdl.handle.net/10568/52074 en Open Access American Meteorological Society Carvalho LMV, Jones C. 2013. CMIP5 Simulations of low-level tropospheric temperature and moisture over the tropical Americas. Journal of Climate 26 (17):6257-6286.
spellingShingle climate
agriculture
monsoon climate
troposphere
models
Carvalho, Leila M. V.
Jones, C.
Posadas, A.
Quiróz, R.
Bookhagen, B.
Liebmann, B.
CMIP5 Simulations of low-level tropospheric temperature and moisture over the tropical Americas
title CMIP5 Simulations of low-level tropospheric temperature and moisture over the tropical Americas
title_full CMIP5 Simulations of low-level tropospheric temperature and moisture over the tropical Americas
title_fullStr CMIP5 Simulations of low-level tropospheric temperature and moisture over the tropical Americas
title_full_unstemmed CMIP5 Simulations of low-level tropospheric temperature and moisture over the tropical Americas
title_short CMIP5 Simulations of low-level tropospheric temperature and moisture over the tropical Americas
title_sort cmip5 simulations of low level tropospheric temperature and moisture over the tropical americas
topic climate
agriculture
monsoon climate
troposphere
models
url https://hdl.handle.net/10568/52074
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