Zobrazeno 1 - 10
of 32
pro vyhledávání: '"Till J. W. Wagner"'
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 10, Pp n/a-n/a (2023)
Abstract At most latitudes, the seasonal cycle of zonal‐mean surface air temperature is notably asymmetric: the length of the warming season is not equal to the length of the cooling season. The asymmetry varies spatially, with the cooling season b
Externí odkaz:
https://doaj.org/article/d2799bab82cc4b039b2b4b7ba4a60afd
Publikováno v:
Journal of Glaciology, Vol 66, Pp 643-657 (2020)
The Antarctic Ice Sheet loses mass via its ice shelves predominantly through two processes: basal melting and iceberg calving. Iceberg calving is episodic and infrequent, and not well parameterized in ice-sheet models. Here, we investigate the impact
Externí odkaz:
https://doaj.org/article/0a5997009523444392212e3fe4373f7c
Publikováno v:
Journal of Climate, vol 35, iss 22
Previous studies have used coupled climate model simulations with perturbed sea ice covers to assess the impact of future Arctic sea ice loss. The results of these studies suggest that Arctic sea ice loss will cause substantial climate impacts in the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::905ece25d53b1b7474634d9ba3561083
https://escholarship.org/uc/item/0288r4qf
https://escholarship.org/uc/item/0288r4qf
Publikováno v:
Journal of Glaciology. 66:643-657
The Antarctic Ice Sheet loses mass via its ice shelves predominantly through two processes: basal melting and iceberg calving. Iceberg calving is episodic and infrequent, and not well parameterized in ice-sheet models. Here, we investigate the impact
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::94873d8f3493f6b26e7306dbdb50b724
https://doi.org/10.1017/jog.2020.35
https://doi.org/10.1017/jog.2020.35
Arctic icebergs, unconstrained sea ice floes, oil slicks, mangrove drifters, lost cargo containers, and other flotsam are known to move at 2-4% of the prevailing wind velocity relative to the water, despite vast differences in the material properties
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::90016605abe582329d34bd896dafb4e3
http://arxiv.org/abs/2201.12688
http://arxiv.org/abs/2201.12688
Publikováno v:
Geophysical Research Letters. 48
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b62e768ff2ec76bd0c5ab69b53b24749
https://doi.org/10.1029/2021gl093069
https://doi.org/10.1029/2021gl093069
Publikováno v:
Geophysical Research Letters. 48
Arctic Amplification is robustly seen in climate model simulations of future warming and in the paleoclimate record. Here, we show that in the instrumental record Arctic Amplification is only a rec...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dc8a65807ba944dd4aeec7b76e37c095
https://doi.org/10.1029/2021gl094086
https://doi.org/10.1029/2021gl094086
Publikováno v:
Reviews of Geophysics. 57:1037-1064
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8f13592e569f5164ea30342f1f2d701f
https://doi.org/10.1029/2018rg000631
https://doi.org/10.1029/2018rg000631
Publikováno v:
Geophysical Research Letters. 48
Annual sea-ice edge phytoplankton blooms occur throughout the Arctic during the spring melt period. Our study considers how phytoplankton spring blooms may depend on sea-ice meltwater. We extend th...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ec77b6c67fd9e1bfc5080258a6e53c92
https://doi.org/10.1029/2020gl091758
https://doi.org/10.1029/2020gl091758
Autor:
Till J. W. Wagner, Laura A. Stevens, Sarah B. Das, Donald Slater, Fiamma Straneo, Hanumant Singh, Clark Richards
Publikováno v:
Wagner, T J W, Straneo, F, Richards, C G, Slater, D A, Stevens, L A, Das, S B & Singh, H 2019, ' Large spatial variations in the flux balance along the front of a Greenland tidewater glacier ', Cryosphere, vol. 13, no. 3, pp. 911-925 . https://doi.org/10.5194/tc-13-911-2019
The Cryosphere, Vol 13, Pp 911-925 (2019)
The Cryosphere, Vol 13, Pp 911-925 (2019)
We acknowledge support from the Woods Hole Oceanographic Institution Ocean and Climate Change Institute Arctic Research Initiative, and NSF OPP-1418256 and OPP-1743693, to Fiamma Straneo and Sarah B. Das. Till J. W. Wagner was further supported by NS
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2e7b9232d6663a75e5f235e21df59c84
https://ora.ox.ac.uk/objects/uuid:d357f374-0160-4d53-9118-04fe3ef2db05
https://ora.ox.ac.uk/objects/uuid:d357f374-0160-4d53-9118-04fe3ef2db05