Pancake sea ice kinematics and dynamics using shipboard stereo video
In the marginal ice zone, surface waves drive motion of sea ice floes. The motion of floes relative to each other can cause periodic collisions, and drives the formation of pancake sea ice. Additionally, the motion of floes relative to the water results in turbulence generation at the interface betw...
Auteurs principaux: | Madison Smith, Jim Thomson |
---|---|
Format: | Article |
Langue: | English |
Publié: |
Cambridge University Press
2020-09-01
|
Collection: | Annals of Glaciology |
Sujets: | |
Accès en ligne: | https://www.cambridge.org/core/product/identifier/S0260305519000351/type/journal_article |
Documents similaires
-
Sea-ice production and air/ice/ocean/biogeochemistry interactions in the Ross Sea during the PIPERS 2017 autumn field campaign
par: S. F. Ackley, et autres
Publié: (2020-09-01) -
Validity of the wave stationarity assumption on estimates of wave attenuation in sea ice: toward a method for wave–ice attenuation observations at global scales
par: Joey J. Voermans, et autres
Publié: (2023-08-01) -
The influence of the spatial distribution of leads and ice floes on the atmospheric boundary layer over fragmented sea ice
par: Marta Wenta, et autres
Publié: (2018-07-01) -
Atmospheric drivers of a winter-to-spring Lagrangian sea-ice drift in the Eastern Antarctic marginal ice zone
par: Ashleigh Womack, et autres
Publié: (2022-10-01) -
An Overview of Antarctic Sea Ice in the Community Earth System Model Version 2, Part I: Analysis of the Seasonal Cycle in the Context of Sea Ice Thermodynamics and Coupled Atmosphere‐Ocean‐Ice Processes
par: Hansi K. A. Singh, et autres
Publié: (2021-03-01)