Sea Spray and Icing in the Emerging Open Water of the Arctic Ocean

With the sea ice cover in the Arctic Ocean declining, the more extensive areas of open water will foster more frequent storms, higher winds, and bigger waves. These conditions can create copious amounts of sea spray. We anticipate that structures placed in shallow water wind turbines or drilling rig...

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Bibliographic Details
Main Author: Andreas, Edgar L
Other Authors: NORTHWEST RESEARCH ASSOCIATES INC BELLEVUE WA
Format: Text
Language:English
Published: 2013
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA582101
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA582101
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spelling ftdtic:ADA582101 2023-05-15T14:54:21+02:00 Sea Spray and Icing in the Emerging Open Water of the Arctic Ocean Andreas, Edgar L NORTHWEST RESEARCH ASSOCIATES INC BELLEVUE WA 2013-06-17 text/html http://www.dtic.mil/docs/citations/ADA582101 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA582101 en eng http://www.dtic.mil/docs/citations/ADA582101 Approved for public release; distribution is unlimited. DTIC Physical and Dynamic Oceanography Snow Ice and Permafrost *ARCTIC OCEAN *OPEN WATER *SEA ICE FREEZING SPRAYS STRUCTURES FIXED OFFSHORE STRUCTURES SEA SPRAY ICING Text 2013 ftdtic 2016-02-24T11:44:10Z With the sea ice cover in the Arctic Ocean declining, the more extensive areas of open water will foster more frequent storms, higher winds, and bigger waves. These conditions can create copious amounts of sea spray. We anticipate that structures placed in shallow water wind turbines or drilling rigs, for instance will, therefore, experience more episodes of freezing spray that will create hazards for both personnel on these structures and for the structures themselves. Few observations, however, have been made of sea spray generation in high winds above, say, 15 20 m/s; and no spray observations have been made in freezing temperatures. Our objective is, thus, to observe the size distribution and rate of creation of spray droplets at air temperatures below freezing and in winds above 15 m/s and, preferably, above 20 m/s. Climatologically, Mt. Desert Rock, a small, well exposed island 24 miles into the Atlantic Ocean from Bar Harbor, Maine, seemed to provide just such conditions in January. Andreas and collaborator Kathy Jones thus spent most of January 2013 observing sea spray and measuring relevant meteorological and ocean conditions on Mt. Desert Rock. We are in the early stages of data analysis but did encounter frequent winds near 20 m/s and temperatures below freezing during our deployment. The original document contains color images. Text Arctic Arctic Ocean Ice permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database Andreas ENVELOPE(-60.729,-60.729,-64.008,-64.008) Arctic Arctic Ocean
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Physical and Dynamic Oceanography
Snow
Ice and Permafrost
*ARCTIC OCEAN
*OPEN WATER
*SEA ICE
FREEZING
SPRAYS
STRUCTURES
FIXED OFFSHORE STRUCTURES
SEA SPRAY ICING
spellingShingle Physical and Dynamic Oceanography
Snow
Ice and Permafrost
*ARCTIC OCEAN
*OPEN WATER
*SEA ICE
FREEZING
SPRAYS
STRUCTURES
FIXED OFFSHORE STRUCTURES
SEA SPRAY ICING
Andreas, Edgar L
Sea Spray and Icing in the Emerging Open Water of the Arctic Ocean
topic_facet Physical and Dynamic Oceanography
Snow
Ice and Permafrost
*ARCTIC OCEAN
*OPEN WATER
*SEA ICE
FREEZING
SPRAYS
STRUCTURES
FIXED OFFSHORE STRUCTURES
SEA SPRAY ICING
description With the sea ice cover in the Arctic Ocean declining, the more extensive areas of open water will foster more frequent storms, higher winds, and bigger waves. These conditions can create copious amounts of sea spray. We anticipate that structures placed in shallow water wind turbines or drilling rigs, for instance will, therefore, experience more episodes of freezing spray that will create hazards for both personnel on these structures and for the structures themselves. Few observations, however, have been made of sea spray generation in high winds above, say, 15 20 m/s; and no spray observations have been made in freezing temperatures. Our objective is, thus, to observe the size distribution and rate of creation of spray droplets at air temperatures below freezing and in winds above 15 m/s and, preferably, above 20 m/s. Climatologically, Mt. Desert Rock, a small, well exposed island 24 miles into the Atlantic Ocean from Bar Harbor, Maine, seemed to provide just such conditions in January. Andreas and collaborator Kathy Jones thus spent most of January 2013 observing sea spray and measuring relevant meteorological and ocean conditions on Mt. Desert Rock. We are in the early stages of data analysis but did encounter frequent winds near 20 m/s and temperatures below freezing during our deployment. The original document contains color images.
author2 NORTHWEST RESEARCH ASSOCIATES INC BELLEVUE WA
format Text
author Andreas, Edgar L
author_facet Andreas, Edgar L
author_sort Andreas, Edgar L
title Sea Spray and Icing in the Emerging Open Water of the Arctic Ocean
title_short Sea Spray and Icing in the Emerging Open Water of the Arctic Ocean
title_full Sea Spray and Icing in the Emerging Open Water of the Arctic Ocean
title_fullStr Sea Spray and Icing in the Emerging Open Water of the Arctic Ocean
title_full_unstemmed Sea Spray and Icing in the Emerging Open Water of the Arctic Ocean
title_sort sea spray and icing in the emerging open water of the arctic ocean
publishDate 2013
url http://www.dtic.mil/docs/citations/ADA582101
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA582101
long_lat ENVELOPE(-60.729,-60.729,-64.008,-64.008)
geographic Andreas
Arctic
Arctic Ocean
geographic_facet Andreas
Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Ice
permafrost
Sea ice
genre_facet Arctic
Arctic Ocean
Ice
permafrost
Sea ice
op_source DTIC
op_relation http://www.dtic.mil/docs/citations/ADA582101
op_rights Approved for public release; distribution is unlimited.
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