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  Northern hemisphere monsoon response to mid-holocene orbital forcing and greenhouse gas-induced global warming

D'Agostino, R., Bader, J., Bordoni, S., Ferreira, D., & Jungclaus, J. H. (2019). Northern hemisphere monsoon response to mid-holocene orbital forcing and greenhouse gas-induced global warming. Geophysical Research Letters, 46, 1591-1601. doi:10.1029/2018GL081589.

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D'Agostino_et_al-2019-Geophysical_Research_Letters.pdf (Publisher version), 2MB
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D'Agostino_et_al-2019-Geophysical_Research_Letters.pdf
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https://esgf-data.dkrz.de/search/cmip5-dkrz/ (Supplementary material)
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D'Agostino, Roberta1, Author           
Bader, Juergen2, Author           
Bordoni, S., Author
Ferreira, D., Author
Jungclaus, Johann H.1, Author                 
Affiliations:
1Director’s Research Group OES, The Ocean in the Earth System, MPI for Meteorology, Max Planck Society, ou_913553              
2Director’s Research Group LES, The Land in the Earth System, MPI for Meteorology, Max Planck Society, ou_913564              

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Free keywords: Budget control; Climate models; Global warming; Greenhouse gases; Moisture; Rain, Hadley circulation; Holocenes; Moisture budget; monsoon; PMIP3-CMIP5, Atmospheric thermodynamics
 Abstract: Precipitation and circulation patterns of Northern Hemisphere monsoons are investigated in Coupled Model Intercomparison Project phase 5 simulations for mid-Holocene and future climate scenario rcp8.5. Although both climates exhibit Northern Hemisphere warming and enhanced interhemispheric thermal contrast in boreal summer, changes in the spatial extent and rainfall intensity in future climate are smaller than in mid-Holocene for all Northern Hemisphere monsoons except the Indian monsoon. A decomposition of the moisture budget in thermodynamic and dynamic contributions suggests that under future global warming, the weaker response of the African, Indian, and North American monsoons results from a compensation between both components. The dynamic component, primarily constrained by changes in net energy input over land, determines instead most of the mid-Holocene land monsoonal rainfall response. ©2019. American Geophysical Union. All Rights Reserved.

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Language(s): eng - English
 Dates: 20192019-02-192019-03-16
 Publication Status: Issued
 Pages: -
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 Table of Contents: -
 Rev. Type: Peer
 Identifiers: DOI: 10.1029/2018GL081589
BibTex Citekey: D'Agostino2019
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Title: Geophysical Research Letters
  Abbreviation : GRL
Source Genre: Journal
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Publ. Info: Washington, D.C. : American Geophysical Union / Wiley
Pages: - Volume / Issue: 46 Sequence Number: - Start / End Page: 1591 - 1601 Identifier: ISSN: 0094-8276
CoNE: https://pure.mpg.de/cone/journals/resource/954925465217