Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Jeremy M. Klavans"'
Publikováno v:
npj Climate and Atmospheric Science, Vol 4, Iss 1, Pp 1-8 (2021)
Abstract The North Atlantic Oscillation (NAO) is predictable in climate models at near-decadal timescales. Predictive skill derives from ocean initialization, which can capture variability internal to the climate system, and from external radiative f
Externí odkaz:
https://doaj.org/article/96e2c3bf8c0f4d6787701274dcf87ec5
Publikováno v:
Journal of Climate. 35:2741-2754
Atlantic multidecadal variability (AMV) impacts temperature, precipitation, and extreme events on both sides of the Atlantic Ocean basin. Previous studies with climate models have suggested that when external radiative forcing is held constant, the l
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9fbefa50bb9eea9dc80216912cc22a1a
https://doi.org/10.1175/jcli-d-21-0338.1
https://doi.org/10.1175/jcli-d-21-0338.1
Autor:
Chengfei He, Amy C. Clement, Mark A. Cane, Lisa N. Murphy, Jeremy M. Klavans, Tyler M. Fenske
Publikováno v:
Geophysical Research Letters. 49
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ebbd1e68b586a9939f395879858b426f
https://doi.org/10.1029/2022gl100420
https://doi.org/10.1029/2022gl100420
Publikováno v:
Journal of Climate. 34:4835-4849
This paper attempts to enhance our understanding of the causes of Atlantic multidecadal variability (AMV). Following the literature, we define the AMV as the SST averaged over the North Atlantic basin, linearly detrended and low-pass filtered. There
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::14978a200f420efbcb2ce8bef5c0f20a
https://doi.org/10.1175/jcli-d-20-0167.1
https://doi.org/10.1175/jcli-d-20-0167.1
Publikováno v:
npj Climate and Atmospheric Science, Vol 4, Iss 1, Pp 1-8 (2021)
The North Atlantic Oscillation (NAO) is predictable in climate models at near-decadal timescales. Predictive skill derives from ocean initialization, which can capture variability internal to the climate system, and from external radiative forcing. H
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d57feda5231612bb51bdbfa7635e423d
https://doaj.org/article/96e2c3bf8c0f4d6787701274dcf87ec5
https://doaj.org/article/96e2c3bf8c0f4d6787701274dcf87ec5
Publikováno v:
Journal of Climate. 32:3847-3864
North Atlantic sea surface temperatures (SST) exhibit a lagged response to the North Atlantic Oscillation (NAO) in both models and observations, which has previously been attributed to changes in ocean heat transport. Here we examine the lagged relat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fcab77b28732836f822b02c295a7f938
https://doi.org/10.1175/jcli-d-18-0409.1
https://doi.org/10.1175/jcli-d-18-0409.1
Autor:
Anton Eisenhauer, Volker Liebetrau, Ralf J. Weger, A. J. Waite, Amy C. Clement, Peter K. Swart, Jeremy M. Klavans, Lisa N. Murphy
The modern history of North Atlantic sea surface temperature shows variability coinciding with changes in air temperature and rainfall over the Northern Hemisphere. There is a debate about this variability and, in particular, whether it is internal t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::70d8e12f9df576ac0c21b7d671d7ac23
https://doi.org/10.1029/2020GL089428
https://doi.org/10.1029/2020GL089428
Publikováno v:
Geophysical Research Letters. 47
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f7de54b6d2c60556dc18f44dc9d25f6b
https://doi.org/10.1029/2020gl088361
https://doi.org/10.1029/2020gl088361
Publikováno v:
Climate Dynamics. 48:3035-3045
Understanding future changes in climate variability, which can impact human activities, is a current research priority. It is often assumed that a key part of this effort involves improving the spatial resolution of climate models; however, few previ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9afb90dcefeeffc29a6780c37d325377
https://doi.org/10.1007/s00382-016-3249-6
https://doi.org/10.1007/s00382-016-3249-6