Zobrazeno 1 - 10
of 12
pro vyhledávání: '"David B. Bonan"'
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 16, Pp n/a-n/a (2024)
Abstract Idealized general circulation models (GCMs) suggest global‐mean precipitation ceases to increase with warming in hot climates because evaporation is limited by the available solar radiation at the surface. We investigate the extent to whic
Externí odkaz:
https://doaj.org/article/e8a19b5e06724a6ebe442a1aa62f2bff
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 11, Pp n/a-n/a (2024)
Abstract State‐of‐the‐art climate models simulate a large spread in the mean‐state Atlantic meridional overturning circulation (AMOC), with strengths varying between 12 and 25 Sv. Here, we introduce a framework for understanding this spread b
Externí odkaz:
https://doaj.org/article/0546740ccaf14b2da0b6ed20d3777707
Autor:
David B. Bonan, Nicole Feldl, Nicholas Siler, Jennifer E. Kay, Kyle C. Armour, Ian Eisenman, Gerard H. Roe
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 3, Pp n/a-n/a (2024)
Abstract The influence of climate feedbacks on regional hydrological changes under warming is poorly understood. Here, a moist energy balance model (MEBM) with a Hadley Cell parameterization is used to isolate the influence of climate feedbacks on ch
Externí odkaz:
https://doaj.org/article/4649afdce60a4420beec719c47634f55
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 23, Pp n/a-n/a (2023)
Abstract Over recent decades, the Southern Ocean (SO) has experienced multi‐decadal surface cooling despite global warming. Earlier studies have proposed that recent SO cooling has been caused by the strengthening of surface westerlies associated w
Externí odkaz:
https://doaj.org/article/5c7c40d94cd346cd9fc4a9358c248ca4
Publikováno v:
Journal of Climate. 36:3499-3522
The response of zonal-mean precipitation minus evaporation (P − E) to global warming is investigated using a moist energy balance model (MEBM) with a simple Hadley cell parameterization. The MEBM accurately emulates zonal-mean P − E change simula
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8d1aa178dc79f7ff250097f92481efaf
https://doi.org/10.1175/jcli-d-22-0337.1
https://doi.org/10.1175/jcli-d-22-0337.1
Publikováno v:
Journal of Climate. 35:5173-5193
The long-term response of the Atlantic meridional overturning circulation (AMOC) to climate change remains poorly understood, in part due to the computational expense associated with running atmosphere–ocean general circulation models (GCMs) to equ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::49596f2f69af79757d110db966eb44f2
https://doi.org/10.1175/jcli-d-21-0912.1
https://doi.org/10.1175/jcli-d-21-0912.1
The Arctic sea ice cover is strongly influenced by internal variability on decadal time scales, affecting both short-term trends and the timing of the first ice-free summer. Several mechanisms of variability have been proposed, but the contributions
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7a505f5b467be5f4968ccc87f0156b73
https://doi.org/10.5194/egusphere-egu23-4159
https://doi.org/10.5194/egusphere-egu23-4159
In response to increased greenhouse-gas concentrations, climate models predict the largest relative change in precipitation will occur in the polar regions, where a substantial absolute increase in precipitation coincides with small precipitation rat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::21220a6ff5dac11d2946ef355b1d2be7
https://doi.org/10.22541/essoar.168319756.61753160/v1
https://doi.org/10.22541/essoar.168319756.61753160/v1
Publikováno v:
eISSN
Antarctic sea ice gradually increased from the late 1970s until 2016, when it experienced an abrupt decline. A number of mechanisms have been proposed for both the gradual increase and abrupt decline of Antarctic sea ice, but how each mechanism manif
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::638276a050216152be426c4b7b22693c
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-750/
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-750/
The Arctic sea ice cover is strongly influenced by internal variability on decadal time scales, affecting both short-term trends and the timing of the first ice-free summer. Several mechanisms of variability have been proposed, but how these mechanis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ad8d12495c274a143ce1bdc2df90c5ef
https://tc.copernicus.org/preprints/tc-2023-29/
https://tc.copernicus.org/preprints/tc-2023-29/