water circulation and sea ice crystal structure in the marginal zone of the Laptev Sea flaw polynya

Features of the surface water circulation near the fast ice edge of the flaw polynya have been investigated on the basis of field measurements in the Laptev Sea during April-May 1999. The conclusion about a convective nature of the measured surface currents with a velocity of up to 62 cm/s is made f...

Full description

Bibliographic Details
Main Authors: Dmitrenko, I. A., Tyshko, K. P., Hölemann, Jens, Eicken, H., Kassens, Heidemarie
Format: Article in Journal/Newspaper
Language:unknown
Published: 2002
Subjects:
Laptev Sea
laptev
Sea ice
Online Access:https://epic.awi.de/id/eprint/13824/
https://hdl.handle.net/10013/epic.24191
id ftawi:oai:epic.awi.de:13824
record_format openpolar
spelling ftawi:oai:epic.awi.de:13824 2023-09-05T13:20:55+02:00 water circulation and sea ice crystal structure in the marginal zone of the Laptev Sea flaw polynya Dmitrenko, I. A. Tyshko, K. P. Hölemann, Jens Eicken, H. Kassens, Heidemarie 2002 https://epic.awi.de/id/eprint/13824/ https://hdl.handle.net/10013/epic.24191 unknown Dmitrenko, I. A. , Tyshko, K. P. , Hölemann, J. orcid:0000-0001-5102-4086 , Eicken, H. and Kassens, H. (2002) water circulation and sea ice crystal structure in the marginal zone of the Laptev Sea flaw polynya , Russian Meteorology and Hydrology, 8 , pp. 49-56 . hdl:10013/epic.24191 EPIC3Russian Meteorology and Hydrology, 8, pp. 49-56 Article peerRev 2002 ftawi 2023-08-22T19:50:49Z Features of the surface water circulation near the fast ice edge of the flaw polynya have been investigated on the basis of field measurements in the Laptev Sea during April-May 1999. The conclusion about a convective nature of the measured surface currents with a velocity of up to 62 cm/s is made from CTD profiles and current records. These currents seem to be part of the circulation cells formed due to the brine rejection during intensive ice formation in the polynya. The spatial ice crystal alignment in the flaw polynya is a result of a quasi-stationary cell water circulation at the edge of the polynya. Article in Journal/Newspaper laptev Laptev Sea Sea ice Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Laptev Sea
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description Features of the surface water circulation near the fast ice edge of the flaw polynya have been investigated on the basis of field measurements in the Laptev Sea during April-May 1999. The conclusion about a convective nature of the measured surface currents with a velocity of up to 62 cm/s is made from CTD profiles and current records. These currents seem to be part of the circulation cells formed due to the brine rejection during intensive ice formation in the polynya. The spatial ice crystal alignment in the flaw polynya is a result of a quasi-stationary cell water circulation at the edge of the polynya.
format Article in Journal/Newspaper
author Dmitrenko, I. A.
Tyshko, K. P.
Hölemann, Jens
Eicken, H.
Kassens, Heidemarie
spellingShingle Dmitrenko, I. A.
Tyshko, K. P.
Hölemann, Jens
Eicken, H.
Kassens, Heidemarie
water circulation and sea ice crystal structure in the marginal zone of the Laptev Sea flaw polynya
author_facet Dmitrenko, I. A.
Tyshko, K. P.
Hölemann, Jens
Eicken, H.
Kassens, Heidemarie
author_sort Dmitrenko, I. A.
title water circulation and sea ice crystal structure in the marginal zone of the Laptev Sea flaw polynya
title_short water circulation and sea ice crystal structure in the marginal zone of the Laptev Sea flaw polynya
title_full water circulation and sea ice crystal structure in the marginal zone of the Laptev Sea flaw polynya
title_fullStr water circulation and sea ice crystal structure in the marginal zone of the Laptev Sea flaw polynya
title_full_unstemmed water circulation and sea ice crystal structure in the marginal zone of the Laptev Sea flaw polynya
title_sort water circulation and sea ice crystal structure in the marginal zone of the laptev sea flaw polynya
publishDate 2002
url https://epic.awi.de/id/eprint/13824/
https://hdl.handle.net/10013/epic.24191
geographic Laptev Sea
geographic_facet Laptev Sea
genre laptev
Laptev Sea
Sea ice
genre_facet laptev
Laptev Sea
Sea ice
op_source EPIC3Russian Meteorology and Hydrology, 8, pp. 49-56
op_relation Dmitrenko, I. A. , Tyshko, K. P. , Hölemann, J. orcid:0000-0001-5102-4086 , Eicken, H. and Kassens, H. (2002) water circulation and sea ice crystal structure in the marginal zone of the Laptev Sea flaw polynya , Russian Meteorology and Hydrology, 8 , pp. 49-56 . hdl:10013/epic.24191
_version_ 1776201555687505920

Similar Items