Zobrazeno 1 - 10
of 36
pro vyhledávání: '"Tobias Bayr"'
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 13, Pp n/a-n/a (2024)
Abstract Observed El Niño‐Southern Oscillation (ENSO) varies between decades with high ENSO amplitude and more extreme Eastern Pacific (EP) El Niño events and decades with low ENSO amplitude and mainly weak El Niño events. Based on experiments w
Externí odkaz:
https://doaj.org/article/1eb80ddeea164c32abf23d54cffb0452
Autor:
Mojib Latif, Tobias Bayr, Joakim Kjellsson, Joke F. Lübbecke, Thomas Martin, Hyacinth C. Nnamchi, Wonsun Park, Abhishek Savita, Jing Sun, Dietmar Dommenget
Publikováno v:
Communications Earth & Environment, Vol 4, Iss 1, Pp 1-10 (2023)
Abstract The globally averaged sea-surface temperature (SST) has steadily increased in the last four decades, consistent with the rising atmospheric greenhouse gas concentrations. Parts of the tropical Pacific exhibited less warming than the global a
Externí odkaz:
https://doaj.org/article/3045955c5d7a4ded91ed1160fab4c827
Autor:
Jake W. Casselman, Joke F. Lübbecke, Tobias Bayr, Wenjuan Huo, Sebastian Wahl, Daniela I. V. Domeisen
Publikováno v:
Weather and Climate Dynamics, 4 (2)
El Niño-Southern Oscillation (ENSO) is a major source for teleconnections, including towards the tropical North Atlantic (TNA) region, whereby TNA sea surface temperatures (SSTs) are positively correlated with ENSO in boreal spring following an ENSO
The amplitude of El Niño/Southern Oscillation (ENSO) varied considerably over the last 140 years, for which we have relatively reliable Sea Surface Temperature (SST) observations over the tropical Pacific. The difference between periods of high and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::53113b3fc532a8f6d1c313066b14e52d
https://doi.org/10.5194/egusphere-egu23-6109
https://doi.org/10.5194/egusphere-egu23-6109
Autor:
Tobias Bayr, Mojib Latif
Two atmospheric feedbacks play an important role in the dynamics of the El Niño/Southern Oscillation (ENSO), namely the amplifying zonal wind feedback and the damping heat flux feedback. Here we investigate how and why both feedbacks change under gl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::917f3d3e0c9d2c605824560f2e2079ab
https://doi.org/10.1007/s00382-022-06454-3
https://doi.org/10.1007/s00382-022-06454-3
The El Niño/Southern Oscillation (ENSO) varied considerably over the last 140 years and the reason of that is under debate. The warm phase of ENSO is termed El Niño, the cold phase La Niña. Here we show that the difference between periods of high
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::987d17074ad421dd5b365715c2597d91
https://doi.org/10.21203/rs.3.rs-2699572/v1
https://doi.org/10.21203/rs.3.rs-2699572/v1
Changes in the background climate are known to affect El Niño–Southern Oscillation (ENSO) by altering feedbacks that control ENSO’s characteristics. Here, the sensitivity of ENSO variability to the background climate is investigated by utilizing
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b1d22abf6b40de6b0e67e5837acb2c41
https://doi.org/10.1175/jcli-d-21-1004.1
https://doi.org/10.1175/jcli-d-21-1004.1
Publikováno v:
Climate Dynamics
There is a long-standing debate on how the El Niño/Southern Oscillation (ENSO) amplitude may change during the twenty-first century in response to global warming. Here we identify the sources of uncertainty in the ENSO amplitude projections in model
Publikováno v:
Climate Dynamics. 56:1681-1697
The growth of El Niño/Southern Oscillation (ENSO) events is determined by the balance between ocean dynamics and thermodynamics. Here we quantify the contribution of the thermodynamic feedbacks to the sea surface temperature (SST) change during ENSO