Increase in the range between wet and dry season precipitation

The water vapour content of the atmosphere has increased as a result of global warming, strengthening the hydrological cycle. An analysis of observational data suggests that wet seasons have become wetter, and dry seasons drier, in recent decades. Global temperatures have risen over the past few dec...

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Published inNature geoscience Vol. 6; no. 4; pp. 263 - 267
Main Authors Chou, Chia, Chiang, John C. H., Lan, Chia-Wei, Chung, Chia-Hui, Liao, Yi-Chun, Lee, Chia-Jung
Format Journal Article
LanguageEnglish
Published London Nature Publishing Group UK 01.04.2013
Nature Publishing Group
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Abstract The water vapour content of the atmosphere has increased as a result of global warming, strengthening the hydrological cycle. An analysis of observational data suggests that wet seasons have become wetter, and dry seasons drier, in recent decades. Global temperatures have risen over the past few decades. The water vapour content of the atmosphere has increased as a result, strengthening the global hydrological cycle 1 , 2 , 3 , 4 . This, in turn, has led to wet regions getting wetter, and dry regions drier 1 , 2 , 3 , 4 , 5 , 6 . Climate model simulations suggest that a similar intensification of existing patterns may also apply to the seasonal cycle of rainfall 7 . Here, we analyse regional and global trends in seasonal precipitation extremes over the past three decades, using a number of global and land-alone observational data sets. We show that globally the annual range of precipitation has increased, largely because wet seasons have become wetter. Although the magnitude of the shift is uncertain, largely owing to limitations inherent in the data sets used, the sign of the tendency is robust. On a regional scale, the tendency for wet seasons to get wetter occurs over climatologically rainier regions. Similarly, the tendency for dry season to get drier is seen in drier regions. Even if the total amount of annual rainfall does not change significantly, the enhancement in the seasonal precipitation cycle could have marked consequences for the frequency of droughts and floods.
AbstractList Global temperatures have risen over the past few decades. The water vapour content of the atmosphere has increased as a result, strengthening the global hydrological cycle. This, in turn, has led to wet regions getting wetter, and dry regions drier. Climate model simulations suggest that a similar intensification of existing patterns may also apply to the seasonal cycle of rainfall. Here, we analyse regional and global trends in seasonal precipitation extremes over the past three decades, using a number of global and land-alone observational data sets. We show that globally the annual range of precipitation has increased, largely because wet seasons have become wetter. Although the magnitude of the shift is uncertain, largely owing to limitations inherent in the data sets used, the sign of the tendency is robust. On a regional scale, the tendency for wet seasons to get wetter occurs over climatologically rainier regions. Similarly, the tendency for dry season to get drier is seen in drier regions. Even if the total amount of annual rainfall does not change significantly, the enhancement in the seasonal precipitation cycle could have marked consequences for the frequency of droughts and floods.
The water vapour content of the atmosphere has increased as a result of global warming, strengthening the hydrological cycle. An analysis of observational data suggests that wet seasons have become wetter, and dry seasons drier, in recent decades. Global temperatures have risen over the past few decades. The water vapour content of the atmosphere has increased as a result, strengthening the global hydrological cycle 1 , 2 , 3 , 4 . This, in turn, has led to wet regions getting wetter, and dry regions drier 1 , 2 , 3 , 4 , 5 , 6 . Climate model simulations suggest that a similar intensification of existing patterns may also apply to the seasonal cycle of rainfall 7 . Here, we analyse regional and global trends in seasonal precipitation extremes over the past three decades, using a number of global and land-alone observational data sets. We show that globally the annual range of precipitation has increased, largely because wet seasons have become wetter. Although the magnitude of the shift is uncertain, largely owing to limitations inherent in the data sets used, the sign of the tendency is robust. On a regional scale, the tendency for wet seasons to get wetter occurs over climatologically rainier regions. Similarly, the tendency for dry season to get drier is seen in drier regions. Even if the total amount of annual rainfall does not change significantly, the enhancement in the seasonal precipitation cycle could have marked consequences for the frequency of droughts and floods.
Author Lan, Chia-Wei
Liao, Yi-Chun
Chiang, John C. H.
Chou, Chia
Lee, Chia-Jung
Chung, Chia-Hui
Author_xml – sequence: 1
  givenname: Chia
  surname: Chou
  fullname: Chou, Chia
  email: chiachou@rcec.sinica.edu.tw
  organization: Research Center for Environmental Changes, Academia Sinica, Department of Atmospheric Sciences, National Taiwan University
– sequence: 2
  givenname: John C. H.
  surname: Chiang
  fullname: Chiang, John C. H.
  organization: Department of Geography and Berkeley Atmospheric Sciences Center, University of California
– sequence: 3
  givenname: Chia-Wei
  surname: Lan
  fullname: Lan, Chia-Wei
  organization: Civil Aeronautics Administration, Ministry of Transportation and Communications
– sequence: 4
  givenname: Chia-Hui
  surname: Chung
  fullname: Chung, Chia-Hui
  organization: Research Center for Environmental Changes, Academia Sinica
– sequence: 5
  givenname: Yi-Chun
  surname: Liao
  fullname: Liao, Yi-Chun
  organization: Research Center for Environmental Changes, Academia Sinica
– sequence: 6
  givenname: Chia-Jung
  surname: Lee
  fullname: Lee, Chia-Jung
  organization: Research Center for Environmental Changes, Academia Sinica
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Snippet The water vapour content of the atmosphere has increased as a result of global warming, strengthening the hydrological cycle. An analysis of observational data...
Global temperatures have risen over the past few decades. The water vapour content of the atmosphere has increased as a result, strengthening the global...
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SubjectTerms 704/106/242
704/106/35
Annual rainfall
Climate models
Driers
Drought
Dry season
Earth Sciences
Earth System Sciences
Floods
Geochemistry
Geology
Geophysics/Geodesy
Global temperatures
Hydrologic cycle
letter
Precipitation
Rainy season
Regional
Seasons
Water vapor
Wet season
Title Increase in the range between wet and dry season precipitation
URI https://link.springer.com/article/10.1038/ngeo1744
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