Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Paloma Trascasa Castro"'
Publikováno v:
Environmental Research Letters, Vol 18, Iss 8, p 084029 (2023)
Atlantic Multidecadal Variability (AMV) modulates El Niño–Southern Oscillation (ENSO) dynamics. Here, we explore the effect of warm (AMV+) and cold (AMV−) AMV conditions on the austral summer teleconnection of ENSO to Australia using idealized s
Externí odkaz:
https://doaj.org/article/5c1d8c755afa4ee289766805c9602a8a
Publikováno v:
XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
Model simulations show a robust increase in ENSO-related precipitation variability in a warmer climate, however whether the characteristics of ENSO events themselves may change in the future remains uncertain.Pacemaker simulations with the EC-Earth3-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f16df954778bf12dad0aec4181450121
Autor:
William Dow, Amanda Maycock, Christine McKenna, Paloma Trascasa Castro, Manoj Joshi, Doug Smith, Adam Blaker
Variability in the Aleutian Low is a known contributor to North Pacific sea surface temperature (SST) variability, but its role in forcing the basin-wide SST anomalies that characterise Pacific Decadal Variability (PDV) is unclear owing to the diffic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::014c35e57caf330b2e648ca0445236b5
https://doi.org/10.5194/egusphere-egu22-8635
https://doi.org/10.5194/egusphere-egu22-8635
Publikováno v:
Earth and Space Science Open Archive
Interactions between ocean basins affect El Niño–Southern Oscillation (ENSO), altering its impacts on society. Here, we explore the effect of Atlantic Multidecadal Variability (AMV) on ENSO behavior using idealized experiments performed with the N
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::aa9e4ab8d9f3f8d3add914bb0ee4863b
Climate change is one of the most serious problems that humans face today, but until now progress in stopping it has been slow. Climate simulations show that Earth will only stop warming when we reach “net zero” emissions. This means that carbon
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c1ca9678430d8795f9e890d85a993e33
https://eprints.whiterose.ac.uk/179419/1/frym-09-672854.pdf
https://eprints.whiterose.ac.uk/179419/1/frym-09-672854.pdf
Publikováno v:
Journal of Climate. 32:6607-6626
The dependence of the winter stratospheric and Euro-Atlantic climate response on ENSO amplitude is investigated using the HadGEM3 model. Experiments are performed with imposed east Pacific sea surface temperature perturbations corresponding to Niño-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::aa031a31a6ef3a0d6b17ef8e6e697604
https://doi.org/10.1175/jcli-d-18-0746.1
https://doi.org/10.1175/jcli-d-18-0746.1