Zobrazeno 1 - 10
of 4 469
pro vyhledávání: '"Arctic sea ice"'
Autor:
David Docquier, François Massonnet, Francesco Ragone, Annelies Sticker, Thierry Fichefet, Stéphane Vannitsem
Publikováno v:
Scientific Reports, Vol 14, Iss 1, Pp 1-16 (2024)
Abstract Arctic sea-ice extent has strongly decreased since the beginning of satellite observations in the late 1970s. While several drivers are known to be implicated, their respective contribution is not fully understood. Here, we apply the Liang-K
Externí odkaz:
https://doaj.org/article/ecb119beada84296b07bb0febe479c93
Publikováno v:
Scientific Reports, Vol 14, Iss 1, Pp 1-10 (2024)
Abstract Simulating and predicting Arctic sea ice accurately remains an academic focus due to the complex and unclear mechanisms of Arctic sea ice variability and model biases. Meanwhile, the relevant forecasting and monitoring authorities are search
Externí odkaz:
https://doaj.org/article/897a2f1c0f6b403bb025784d5a6a8a46
Publikováno v:
Gaoyuan qixiang, Vol 43, Iss 2, Pp 318-328 (2024)
Using the observed precipitation data of 154 meteorological stations in East of Northwest China， NCEP/NCAR atmosphere reanalysis and Arctic sea ice data from 1961 to 2020， the possible impacts and mechanisms of the key area Arctic sea ice on the
Externí odkaz:
https://doaj.org/article/37fd677361db486ca2515a026ebc154f
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 14, Pp n/a-n/a (2024)
Abstract The state and fate of snow on sea ice are crucial in the mass and energy balance of sea ice. The function of atmospheric rivers (ARs) on snow depth over sea ice has not been measured thus far, limiting the understanding of the mechanism of s
Externí odkaz:
https://doaj.org/article/82b7b097876e4a458471beea7f496fce
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 13, Pp n/a-n/a (2024)
Abstract A novel sub‐sampling method has been used to isolate the dynamic effects of the response of the North Atlantic Oscillation (NAO) and the Siberian High (SH) from the total response to projected Arctic sea‐ice loss under 2°C global warmin
Externí odkaz:
https://doaj.org/article/8a9d40353fba4baa822118a7d5ae66f6
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 12, Pp n/a-n/a (2024)
Abstract Freezing temperature parameterization significantly impacts the heat balance at sea‐ice bottom and, consequently, the simulated sea‐ice thickness. Here, the single‐column model ICEPACK was used to investigate the impact of the freezing
Externí odkaz:
https://doaj.org/article/0175dca28c4d4f50ba036ae743c77137
Publikováno v:
Weather and Climate Extremes, Vol 44, Iss , Pp 100674- (2024)
During 2020, the Arctic is marked by extremely low sea ice coverage and hot climate. September Sea Ice Extent (SIE) was about 2.3 million km2 below the 1979–2014 mean and the 2nd lowest on the 1979–2020 record, while regional summer (June–Augus
Externí odkaz:
https://doaj.org/article/a4295880bd6e4aafa8bc8889fcc574ff
Autor:
Qing-Quan Li, Miao Bi, Song Yang, Qing-Yuan Wu, Yi-Hui Ding, Xin-Yong Shen, Xiao-Ting Sun, Meng-Chu Zhao
Publikováno v:
Advances in Climate Change Research, Vol 15, Iss 1, Pp 42-51 (2024)
The Tibetan Plateau (TP) and the Arctic are the most sensitive regions to global climate change. However, the interdecadal varibility of winter extreme precipitation over the TP and its linkage with Arctic sea ice are still unclear. In this study, th
Externí odkaz:
https://doaj.org/article/4ad51be9cf304c898c4b9b160409b32e
Autor:
Xue Wang, Ran Lu, Shao-Yin Wang, Run-Tong Chen, Zhuo-Qi Chen, Feng-Ming Hui, Hua-Bing Huang, Xiao Cheng
Publikováno v:
Advances in Climate Change Research, Vol 14, Iss 5, Pp 691-706 (2023)
Sea ice drift is a critical parameter for understanding the rapid changes in Arctic sea ice. Since the release of the Coupled Model Intercomparison Project Phase 6 (CMIP6), there has been a lack of quantitative analysis regarding CMIP6's simulation o
Externí odkaz:
https://doaj.org/article/46e89d520e95416ead25f57c02e17e2f
Publikováno v:
Earth's Future, Vol 11, Iss 10, Pp n/a-n/a (2023)
Abstract The ice‐free Arctic in summer not only symbolizes human‐induced climate change but also highlights the need to critically consider climate change adaptation policies. To constrain projections when the Arctic Ocean will first become ice
Externí odkaz:
https://doaj.org/article/c5d32bd2f3b14668a8d2cc9c21dce4b0