A concept for autonomous and continuous observation of melt pond morphology: Instrument design and test trail during the 4th CHINARE-Arctic in 2010
Accelerated decline of summer and winter Arctic sea ice has been demonstrated progressively. Melt ponds play a key role in enhancing the feedback of solar radiation in the ice/ocean-atmosphere system, and have thus been a focus of researchers and modelers. A new melt pond investigation system was de...
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Polar Research Institute of China - PRIC
2011
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ftarcticportal:oai:generic.eprints.org:2438 2023-10-09T21:44:11+02:00 A concept for autonomous and continuous observation of melt pond morphology: Instrument design and test trail during the 4th CHINARE-Arctic in 2010 Wenfeng, Huang Zhijun, Li Yongxue, Wang Ruibo, Lei 2011-12 application/pdf http://library.arcticportal.org/2438/ http://library.arcticportal.org/2438/1/A20110409.pdf en eng Polar Research Institute of China - PRIC http://library.arcticportal.org/2438/1/A20110409.pdf Wenfeng, Huang and Zhijun, Li and Yongxue, Wang and Ruibo, Lei (2011) A concept for autonomous and continuous observation of melt pond morphology: Instrument design and test trail during the 4th CHINARE-Arctic in 2010. Advances in Polar Science, 22 (4). pp. 273-280. Atmosphere Oceans Article PeerReviewed 2011 ftarcticportal 2023-09-20T22:54:11Z Accelerated decline of summer and winter Arctic sea ice has been demonstrated progressively. Melt ponds play a key role in enhancing the feedback of solar radiation in the ice/ocean-atmosphere system, and have thus been a focus of researchers and modelers. A new melt pond investigation system was designed to determine morphologic and hydrologic features, and their evolution. This system consists of three major parts: Temperature-salinity measuring, surface morphology monitoring, and water depth monitoring units. The setup was deployed during the ice camp period of the fourth Chinese National Arctic Research Expedition in summer 2010. The evolution of a typical Arctic melt pond was documented in terms of pond depth, shape and surface condition. These datasets are presented to scientifically reveal how involved parameters change, contributing to better understanding of the evolution mechanism of the melt pond. The main advantage of this system is its suitability for autonomous and long-term observation, over and within a melt pond. Further, the setup is portable and robust. It can be easily and quickly installed, which is most valuable for deployment under harsh conditions. Article in Journal/Newspaper Advances in Polar Science Arctic Arctic Polar Science Polar Science Sea ice Arctic Portal Library Arctic |
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Open Polar |
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Arctic Portal Library |
op_collection_id |
ftarcticportal |
language |
English |
topic |
Atmosphere Oceans |
spellingShingle |
Atmosphere Oceans Wenfeng, Huang Zhijun, Li Yongxue, Wang Ruibo, Lei A concept for autonomous and continuous observation of melt pond morphology: Instrument design and test trail during the 4th CHINARE-Arctic in 2010 |
topic_facet |
Atmosphere Oceans |
description |
Accelerated decline of summer and winter Arctic sea ice has been demonstrated progressively. Melt ponds play a key role in enhancing the feedback of solar radiation in the ice/ocean-atmosphere system, and have thus been a focus of researchers and modelers. A new melt pond investigation system was designed to determine morphologic and hydrologic features, and their evolution. This system consists of three major parts: Temperature-salinity measuring, surface morphology monitoring, and water depth monitoring units. The setup was deployed during the ice camp period of the fourth Chinese National Arctic Research Expedition in summer 2010. The evolution of a typical Arctic melt pond was documented in terms of pond depth, shape and surface condition. These datasets are presented to scientifically reveal how involved parameters change, contributing to better understanding of the evolution mechanism of the melt pond. The main advantage of this system is its suitability for autonomous and long-term observation, over and within a melt pond. Further, the setup is portable and robust. It can be easily and quickly installed, which is most valuable for deployment under harsh conditions. |
format |
Article in Journal/Newspaper |
author |
Wenfeng, Huang Zhijun, Li Yongxue, Wang Ruibo, Lei |
author_facet |
Wenfeng, Huang Zhijun, Li Yongxue, Wang Ruibo, Lei |
author_sort |
Wenfeng, Huang |
title |
A concept for autonomous and continuous observation of melt pond morphology: Instrument design and test trail during the 4th CHINARE-Arctic in 2010 |
title_short |
A concept for autonomous and continuous observation of melt pond morphology: Instrument design and test trail during the 4th CHINARE-Arctic in 2010 |
title_full |
A concept for autonomous and continuous observation of melt pond morphology: Instrument design and test trail during the 4th CHINARE-Arctic in 2010 |
title_fullStr |
A concept for autonomous and continuous observation of melt pond morphology: Instrument design and test trail during the 4th CHINARE-Arctic in 2010 |
title_full_unstemmed |
A concept for autonomous and continuous observation of melt pond morphology: Instrument design and test trail during the 4th CHINARE-Arctic in 2010 |
title_sort |
concept for autonomous and continuous observation of melt pond morphology: instrument design and test trail during the 4th chinare-arctic in 2010 |
publisher |
Polar Research Institute of China - PRIC |
publishDate |
2011 |
url |
http://library.arcticportal.org/2438/ http://library.arcticportal.org/2438/1/A20110409.pdf |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Advances in Polar Science Arctic Arctic Polar Science Polar Science Sea ice |
genre_facet |
Advances in Polar Science Arctic Arctic Polar Science Polar Science Sea ice |
op_relation |
http://library.arcticportal.org/2438/1/A20110409.pdf Wenfeng, Huang and Zhijun, Li and Yongxue, Wang and Ruibo, Lei (2011) A concept for autonomous and continuous observation of melt pond morphology: Instrument design and test trail during the 4th CHINARE-Arctic in 2010. Advances in Polar Science, 22 (4). pp. 273-280. |
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1779319990016540672 |