Atmospheric forcing of wave states in the southeast Chukchi Sea

Dissertation (Ph.D.) University of Alaska Fairbanks, 2012 The objective of this study was to assess the impact that the ocean state, particularly ocean waves, have on coastal communities and operations in the Western Alaska region. In situ measurements and one-dimensional spectra models, were used t...

Full description

Bibliographic Details
Main Author: Francis, Oceana Puananilei
Other Authors: Atkinson, David, Bhatt, Uma, Metzger, Andrew, Walsh, John, Weingartner, Thomas
Format: Doctoral or Postdoctoral Thesis
Language:unknown
Published: 2012
Subjects:
Online Access:http://hdl.handle.net/11122/5891
id ftunivalaska:oai:scholarworks.alaska.edu:11122/5891
record_format openpolar
spelling ftunivalaska:oai:scholarworks.alaska.edu:11122/5891 2023-05-15T15:02:17+02:00 Atmospheric forcing of wave states in the southeast Chukchi Sea Francis, Oceana Puananilei Atkinson, David Bhatt, Uma Metzger, Andrew Walsh, John Weingartner, Thomas 2012-05 http://hdl.handle.net/11122/5891 unknown http://hdl.handle.net/11122/5891 Department of Atmospheric Sciences Dissertation phd 2012 ftunivalaska 2023-02-23T21:36:31Z Dissertation (Ph.D.) University of Alaska Fairbanks, 2012 The objective of this study was to assess the impact that the ocean state, particularly ocean waves, have on coastal communities and operations in the Western Alaska region. In situ measurements and one-dimensional spectra models, were used to link observed wave activity – wind-sea and swells – to their synoptic drivers. Bottommounted Recording Doppler Current Profilers (RDCPs) were placed at offshore and nearshore locations in the southeast Chukchi Sea, Alaska, during 2007 and 2009-2010. The highest significant wave height (SWH) “events” were defined as wave heights above 2m and 3m for a duration of 6h or more. Results show that SWH events appeared to be driven by three types of systems, 1) cyclonic systems that moved into the eastern Bering Sea and then stalled there, 2) cyclonic systems that moved into the eastern Chukchi Sea and then loitered there, and 3) a cyclonic system over the Brooks Range, a less common occurrence. Results also show the offshore region having highest SWHs with an east wind and wave direction, and classified as a wind-sea state. For the nearshore region, highest SWHs with south and west wind and wave directions, generally showed a swell state. Agreement between one-dimensional spectral models and in situ measurements was greatest for the higher wind-sea state in the offshore region, while discrepancies arose for the lower swell state in the nearshore region. Cross-validation of in situ measurements with satellite altimeter radar measurements were also conducted. Good correlation was found for the offshore regions iv but not for the nearshore regions. Satellite observations were also used to assess wave conditions in the Arctic during the years 1993-2011. A 0.020m/year increase of SWH for the SE Chukchi Sea and a 0.025m/year increase for the Pacific-Arctic, was found which correlates well with diminishing sea ice and the heighted wind speed, also shown in this study. Signature Page -- Title Page -- Abstract -- Dedication -- ... Doctoral or Postdoctoral Thesis Arctic Bering Sea Brooks Range Chukchi Chukchi Sea Pacific Arctic Sea ice Alaska University of Alaska: ScholarWorks@UA Arctic Bering Sea Chukchi Sea Fairbanks Pacific
institution Open Polar
collection University of Alaska: ScholarWorks@UA
op_collection_id ftunivalaska
language unknown
description Dissertation (Ph.D.) University of Alaska Fairbanks, 2012 The objective of this study was to assess the impact that the ocean state, particularly ocean waves, have on coastal communities and operations in the Western Alaska region. In situ measurements and one-dimensional spectra models, were used to link observed wave activity – wind-sea and swells – to their synoptic drivers. Bottommounted Recording Doppler Current Profilers (RDCPs) were placed at offshore and nearshore locations in the southeast Chukchi Sea, Alaska, during 2007 and 2009-2010. The highest significant wave height (SWH) “events” were defined as wave heights above 2m and 3m for a duration of 6h or more. Results show that SWH events appeared to be driven by three types of systems, 1) cyclonic systems that moved into the eastern Bering Sea and then stalled there, 2) cyclonic systems that moved into the eastern Chukchi Sea and then loitered there, and 3) a cyclonic system over the Brooks Range, a less common occurrence. Results also show the offshore region having highest SWHs with an east wind and wave direction, and classified as a wind-sea state. For the nearshore region, highest SWHs with south and west wind and wave directions, generally showed a swell state. Agreement between one-dimensional spectral models and in situ measurements was greatest for the higher wind-sea state in the offshore region, while discrepancies arose for the lower swell state in the nearshore region. Cross-validation of in situ measurements with satellite altimeter radar measurements were also conducted. Good correlation was found for the offshore regions iv but not for the nearshore regions. Satellite observations were also used to assess wave conditions in the Arctic during the years 1993-2011. A 0.020m/year increase of SWH for the SE Chukchi Sea and a 0.025m/year increase for the Pacific-Arctic, was found which correlates well with diminishing sea ice and the heighted wind speed, also shown in this study. Signature Page -- Title Page -- Abstract -- Dedication -- ...
author2 Atkinson, David
Bhatt, Uma
Metzger, Andrew
Walsh, John
Weingartner, Thomas
format Doctoral or Postdoctoral Thesis
author Francis, Oceana Puananilei
spellingShingle Francis, Oceana Puananilei
Atmospheric forcing of wave states in the southeast Chukchi Sea
author_facet Francis, Oceana Puananilei
author_sort Francis, Oceana Puananilei
title Atmospheric forcing of wave states in the southeast Chukchi Sea
title_short Atmospheric forcing of wave states in the southeast Chukchi Sea
title_full Atmospheric forcing of wave states in the southeast Chukchi Sea
title_fullStr Atmospheric forcing of wave states in the southeast Chukchi Sea
title_full_unstemmed Atmospheric forcing of wave states in the southeast Chukchi Sea
title_sort atmospheric forcing of wave states in the southeast chukchi sea
publishDate 2012
url http://hdl.handle.net/11122/5891
geographic Arctic
Bering Sea
Chukchi Sea
Fairbanks
Pacific
geographic_facet Arctic
Bering Sea
Chukchi Sea
Fairbanks
Pacific
genre Arctic
Bering Sea
Brooks Range
Chukchi
Chukchi Sea
Pacific Arctic
Sea ice
Alaska
genre_facet Arctic
Bering Sea
Brooks Range
Chukchi
Chukchi Sea
Pacific Arctic
Sea ice
Alaska
op_relation http://hdl.handle.net/11122/5891
Department of Atmospheric Sciences
_version_ 1766334253142900736