Vertical mixing in the Arctic Ocean inferred from eXpendable Current Profilers

Recent and historical data sets from different regions of the Arctic Ocean are analysed using velocity profiles from 127 eXpendable Current Profiler (XCP) deployments from the time period 1993 to 2010. The data sets are processed identically. The shear profiles of horizontal velocity are used to inf...

Full description

Bibliographic Details
Main Author: Meyer, Anja Kristiansen
Format: Master Thesis
Language:English
Published: The University of Bergen 2011
Subjects:
Online Access:https://hdl.handle.net/1956/5132
id ftunivbergen:oai:bora.uib.no:1956/5132
record_format openpolar
spelling ftunivbergen:oai:bora.uib.no:1956/5132 2023-05-15T14:51:12+02:00 Vertical mixing in the Arctic Ocean inferred from eXpendable Current Profilers Meyer, Anja Kristiansen 2011-05-31 7940320 bytes application/pdf https://hdl.handle.net/1956/5132 eng eng The University of Bergen https://hdl.handle.net/1956/5132 Vertical mixing Physical oceanography eXpendable Current Profilers Arctic ocean 756213 VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452 Master thesis 2011 ftunivbergen 2023-03-14T17:43:40Z Recent and historical data sets from different regions of the Arctic Ocean are analysed using velocity profiles from 127 eXpendable Current Profiler (XCP) deployments from the time period 1993 to 2010. The data sets are processed identically. The shear profiles of horizontal velocity are used to infer vertical mixing. Using the fine-scale parameterization which relate internal wave energy to energy dissipation rate, the diapycnal eddy diffusivity is inferred. An improved version of the fine-scale parameterization which includes corrections for the shear-strain ratio and variation in latitude is also employed. Joint microstructure measurements made it possible to compare the XCP derived eddy diffusivity with direct observations to test the applicability of the parameterization. It is concluded that the skill of the XCP derived eddy diffusivity in the Arctic Ocean is within a factor of 5-6. Using XCP deployments done at the same time and same location the accuracy of the eddy diffusivity calculation is estimated to be within one order of magnitude. The eddy diffusivity values are compared in relation to topographic variations and temporal variability. For the deeper layers of the ocean, the eddy diffusivity values averaged for slope and ridge areas are comparable, and a factor of two higher than those for the abyss. The analysis on the temporal variability was inconclusive due to relatively poor quality data set from 1993. Master i Meteorologi og oseanografi MAMN-GEOF GEOF399 Master Thesis Arctic Arctic Ocean University of Bergen: Bergen Open Research Archive (BORA-UiB) Arctic Arctic Ocean
institution Open Polar
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
op_collection_id ftunivbergen
language English
topic Vertical mixing
Physical oceanography
eXpendable Current Profilers
Arctic ocean
756213
VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452
spellingShingle Vertical mixing
Physical oceanography
eXpendable Current Profilers
Arctic ocean
756213
VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452
Meyer, Anja Kristiansen
Vertical mixing in the Arctic Ocean inferred from eXpendable Current Profilers
topic_facet Vertical mixing
Physical oceanography
eXpendable Current Profilers
Arctic ocean
756213
VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452
description Recent and historical data sets from different regions of the Arctic Ocean are analysed using velocity profiles from 127 eXpendable Current Profiler (XCP) deployments from the time period 1993 to 2010. The data sets are processed identically. The shear profiles of horizontal velocity are used to infer vertical mixing. Using the fine-scale parameterization which relate internal wave energy to energy dissipation rate, the diapycnal eddy diffusivity is inferred. An improved version of the fine-scale parameterization which includes corrections for the shear-strain ratio and variation in latitude is also employed. Joint microstructure measurements made it possible to compare the XCP derived eddy diffusivity with direct observations to test the applicability of the parameterization. It is concluded that the skill of the XCP derived eddy diffusivity in the Arctic Ocean is within a factor of 5-6. Using XCP deployments done at the same time and same location the accuracy of the eddy diffusivity calculation is estimated to be within one order of magnitude. The eddy diffusivity values are compared in relation to topographic variations and temporal variability. For the deeper layers of the ocean, the eddy diffusivity values averaged for slope and ridge areas are comparable, and a factor of two higher than those for the abyss. The analysis on the temporal variability was inconclusive due to relatively poor quality data set from 1993. Master i Meteorologi og oseanografi MAMN-GEOF GEOF399
format Master Thesis
author Meyer, Anja Kristiansen
author_facet Meyer, Anja Kristiansen
author_sort Meyer, Anja Kristiansen
title Vertical mixing in the Arctic Ocean inferred from eXpendable Current Profilers
title_short Vertical mixing in the Arctic Ocean inferred from eXpendable Current Profilers
title_full Vertical mixing in the Arctic Ocean inferred from eXpendable Current Profilers
title_fullStr Vertical mixing in the Arctic Ocean inferred from eXpendable Current Profilers
title_full_unstemmed Vertical mixing in the Arctic Ocean inferred from eXpendable Current Profilers
title_sort vertical mixing in the arctic ocean inferred from expendable current profilers
publisher The University of Bergen
publishDate 2011
url https://hdl.handle.net/1956/5132
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
genre_facet Arctic
Arctic Ocean
op_relation https://hdl.handle.net/1956/5132
_version_ 1766322252401344512