Zobrazeno 1 - 10
of 501
pro vyhledávání: '"Gerrit Lohmann"'
Autor:
Yong Sun, Haibin Wu, Lin Ding, Lixin Chen, Christian Stepanek, Yan Zhao, Ning Tan, Baohuang Su, Xiayu Yuan, Wenchao Zhang, Bo Liu, Stephen Hunter, Alan Haywood, Ayako Abe-Ouchi, Bette Otto-Bliesner, Camille Contoux, Daniel J. Lunt, Aisling Dolan, Deepak Chandan, Gerrit Lohmann, Harry Dowsett, Julia Tindall, Michiel Baatsen, W. Richard Peltier, Qiang Li, Ran Feng, Ulrich Salzmann, Wing-Le Chan, Zhongshi Zhang, Charles J. R. Williams, Gilles Ramstein
Publikováno v:
npj Climate and Atmospheric Science, Vol 7, Iss 1, Pp 1-10 (2024)
Abstract The mid-Piacenzian warm period (MPWP, ~3.264–3.025 Ma) has gained widespread interest due to its partial analogy with future climate. However, quantitative data–model comparison of East Asian Summer Monsoon (EASM) precipitation during th
Externí odkaz:
https://doaj.org/article/a17bf41105bb4dd0bbb313e85f2643de
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 16, Pp n/a-n/a (2024)
Abstract The last deglaciation experienced the retreat of massive ice sheets and a transition from the cold Last Glacial Maximum to the warmer Holocene. Key simulation challenges for this period include the timing and extent of ice sheet decay and me
Externí odkaz:
https://doaj.org/article/a3ee24d3689b429a9ce794f8b9cb3074
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 12, Pp n/a-n/a (2024)
Abstract The last glacial inception (LGI) marks the transition from the interglacial warm climate to the glacial period with extensive Northern Hemisphere ice sheets and colder climate. This transition is initiated by decreasing boreal summer insolat
Externí odkaz:
https://doaj.org/article/e6a8a98890be42e1964fda9e20320f6a
Autor:
Jian Shi, Gerrit Lohmann
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 4, Pp n/a-n/a (2024)
Abstract Arctic temperature is one of the most uncertain aspects of mid‐Holocene (MH) climate change modeling, usually attributed to the different responses of different models to external forcing. However, in this study, we find that significant d
Externí odkaz:
https://doaj.org/article/75bf4604a2394e969dd5f9e3c5ddd0ca
Publikováno v:
Frontiers in Climate, Vol 6 (2024)
While the Arctic's accelerated warming and sea ice decline have been associated with Eurasian cooling, debates persist between those attributing this to sea ice retreat and those to internal variability. Our study examines the association between aut
Externí odkaz:
https://doaj.org/article/efb2226425a1463db2e48ec94c9ad3e7
Publikováno v:
Scientific Reports, Vol 13, Iss 1, Pp 1-18 (2023)
Abstract Climate indices are often used as a climate monitoring tool, allowing us to understand how the frequency, intensity, and duration of extreme weather events are changing over time. Here, based on complex statistical analysis we identify highl
Externí odkaz:
https://doaj.org/article/4cd0bf5f10b2473baebfa0e80ba6460e
Publikováno v:
Journal of Water and Climate Change, Vol 14, Iss 9, Pp 3112-3130 (2023)
The objective of this study is to analyze and visualize the spatial distribution of trends for 74 climate indices on a monthly time-scale in direction, magnitude, and significance level at a resolution of 0.1° during the period of 1950–2021 over t
Externí odkaz:
https://doaj.org/article/3a031eb329484a599fb793c142eafc9b
Publikováno v:
Journal of Glaciology, Vol 69, Pp 1056-1070 (2023)
Spatially variable basal conditions are thought to govern how ice sheets behave at glacial time scales (>1000 years) and responsible for changes in dynamics between the core and peripheral regions of the Laurentide and Fennoscandian ice sheets. Basal
Externí odkaz:
https://doaj.org/article/779fe7048a96419c86cf931a68a14d11
Autor:
Hu Yang, Gerrit Lohmann, Christian Stepanek, Qiang Wang, Rui Xin Huang, Xiaoxu Shi, Jiping Liu, Dake Chen, Xulong Wang, Yi Zhong, Qinghua Yang, Ying Bao, Juliane Müller
Publikováno v:
Communications Earth & Environment, Vol 4, Iss 1, Pp 1-10 (2023)
Abstract Satellite observations covering the last four decades reveal an ocean warming pattern resembling the negative phase of the Pacific Decadal Oscillation. This pattern has therefore been widely interpreted as a manifestation of natural climate
Externí odkaz:
https://doaj.org/article/bf8e3340d5d8430ba071ebfcb7b3b7ac
Publikováno v:
PLoS ONE, Vol 19, Iss 4, p e0300138 (2024)
Using the climate model CLIMBER-X, we present an efficient method for assimilating the temporal evolution of surface temperatures for the last deglaciation covering the period 22000 to 6500 years before the present. The data assimilation methodology
Externí odkaz:
https://doaj.org/article/6e947d016fb1402ca897abff18f7da1a