Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Tasha Snow"'
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 22, Pp n/a-n/a (2023)
Abstract Open ocean areas surrounded by sea ice and maintained by ocean heat, or sensible‐heat polynyas, are linked to key ice‐sheet processes, such as ice‐shelf basal melt and ice‐shelf fracture, when they occur near ice‐shelf fronts. Howe
Externí odkaz:
https://doaj.org/article/c253500752b94cef931a63bea249432d
Autor:
Tiago S. Dotto, Karen J. Heywood, Rob A. Hall, Ted A. Scambos, Yixi Zheng, Yoshihiro Nakayama, Shuntaro Hyogo, Tasha Snow, Anna K. Wåhlin, Christian Wild, Martin Truffer, Atsuhiro Muto, Karen E. Alley, Lars Boehme, Guilherme A. Bortolotto, Scott W. Tyler, Erin Pettit
Publikováno v:
Nature Communications, Vol 13, Iss 1, Pp 1-13 (2022)
A weaker ocean gyre in the Pine Island Bay, suppressed by higher sea-ice concentration over the ocean near the Thwaites Eastern Ice Shelf, allows more meltwater to enter the sub-ice-shelf cavity. This increases the ocean temperature beneath the ice.
Externí odkaz:
https://doaj.org/article/476b9ec7aa364f58aba55435b2af040c
Autor:
Karen E. Alley, Richard B. Alley, Alex D. Crawford, Naomi Ochwat, Christian T. Wild, Juliana Marson, Tasha Snow, Atsuhiro Muto, Erin C. Pettit, Sarah F. Child, Martin Truffer, Gabriela Collao-Barrios, Ted A. Scambos
Publikováno v:
Journal of Glaciology, Pp 1-15
Basal channels, which are troughs carved into the undersides of ice shelves by buoyant plumes of water, are modulators of ice-shelf basal melt and structural stability. In this study, we track the evolution of 12 large basal channels beneath ice shel
Externí odkaz:
https://doaj.org/article/9d3b4025915648598961db0373808eb4
Autor:
Elena Savidge, Tasha Snow, Matthew R. Siegfried, Yixi Zheng, Ana B. Villas Bôas, Guilherme A. Bortolotto, Lars Boehme, Karen E. Alley
Funding: This work was enabled by the NSF-NERC International Thwaites Glacier Collaboration: Thwaites-Amundsen Regional Survey and Network (ITGC: TARSAN; NERC Grant: NE/S006419/1, NE/S006591/1, NSF Grant: 1738992) and the NERC Ice Sheet Stability Pro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5524cc8efa6df6b080dd676c349313d3
https://hdl.handle.net/10023/27482
https://hdl.handle.net/10023/27482
Autor:
Ellianna Abrahams, Tasha Snow, Eojin Lee, Elena Savidge, Matthew R. Siegfried, Fernando Pérez
Sensible-heat polynyas, i.e. persistent polynyas produced thermodynamically, can form across multiple years where relatively warm water flows out from the sub-ice-shelf cavity toward ice shelf fronts, typically directed by channels carved into the ic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::17706311df011cced813d33b1d85d0ef
https://doi.org/10.5194/egusphere-egu23-16994
https://doi.org/10.5194/egusphere-egu23-16994
This document is the CryoCloud leadership team's response to NNH23ZDA005LRequest for Information: Scientific Data and Computing Architecture to Support Open Science. Insupport of open scientific research and development processes via the Open-Source
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ba0152d784395c3a1af02c407ae1fc72
Autor:
Tasha Snow, Joanna Millstein, Wei Ji Leong, Jessica Scheick, Wilson Sauthoff, James Colliander, James Munroe, Fernando Perez, Yuvi Panda, Denis Felikson, Tyler Sutterley, Matthew Siegfried
Slides for the onboarding training for users of the CryoCloud JupyterHub. This presentation was recorded in a video (https://youtu.be/QNrDlwiomgc) that provides information about the CryoCloud project, how to contribute to the community, a demo for a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3876ca3ae2dff5317b806cc82962681d
Autor:
Tiago Dotto, Karen Heywood, Rob Hall, Ted Scambos, Yixi Zheng, Yoshihiro Nakayama, Tasha Snow, Anna Wåhlin, Christian Wild, Martin Truffer, Atsuhiro Muto, Erin Pettit
Basal melting of the Amundsen Sea ice shelves is caused by relatively warm waters accessing the ice base through turbulent processes at the ice-ocean boundary layer. Here we report hydrographic variability in Thwaites Eastern Ice Shelf (TEIS) from Ja
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::254865a33726a74ef143d1fdce3f1f78
https://doi.org/10.5194/egusphere-egu22-817
https://doi.org/10.5194/egusphere-egu22-817