On the impact of high-resolution, high-frequency meteorological forcing on Denmark Strait ocean circulation
This paper quantifies and discusses the impact of high-resolution, high-frequency atmospheric forcing on the ocean circulation in the vicinity of the Denmark Strait. The approach is to force a 2 km resolution regional ocean circulation model with atmospheric states from reanalysis products that have...
Published in: | Quarterly Journal of the Royal Meteorological Society |
---|---|
Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2009
|
Subjects: | |
Online Access: | https://ueaeprints.uea.ac.uk/id/eprint/24326/ https://ueaeprints.uea.ac.uk/id/eprint/24326/1/haine_etal_met_forcing_ocean_QJRMS_2009.pdf https://doi.org/10.1002/qj.505 |
id |
ftuniveastangl:oai:ueaeprints.uea.ac.uk:24326 |
---|---|
record_format |
openpolar |
spelling |
ftuniveastangl:oai:ueaeprints.uea.ac.uk:24326 2023-05-15T16:00:36+02:00 On the impact of high-resolution, high-frequency meteorological forcing on Denmark Strait ocean circulation Haine, T. W. N. Zhang, S. Moore, G. W. K. Renfrew, I. A. 2009-10 application/pdf https://ueaeprints.uea.ac.uk/id/eprint/24326/ https://ueaeprints.uea.ac.uk/id/eprint/24326/1/haine_etal_met_forcing_ocean_QJRMS_2009.pdf https://doi.org/10.1002/qj.505 en eng https://ueaeprints.uea.ac.uk/id/eprint/24326/1/haine_etal_met_forcing_ocean_QJRMS_2009.pdf Haine, T. W. N., Zhang, S., Moore, G. W. K. and Renfrew, I. A. (2009) On the impact of high-resolution, high-frequency meteorological forcing on Denmark Strait ocean circulation. Quarterly Journal of the Royal Meteorological Society, 135 (645). pp. 2067-2085. ISSN 1477-870X doi:10.1002/qj.505 Article PeerReviewed 2009 ftuniveastangl https://doi.org/10.1002/qj.505 2023-03-23T23:31:28Z This paper quantifies and discusses the impact of high-resolution, high-frequency atmospheric forcing on the ocean circulation in the vicinity of the Denmark Strait. The approach is to force a 2 km resolution regional ocean circulation model with atmospheric states from reanalysis products that have different spatial and temporal resolutions. We use the National Center for Environmental Prediction global reanalysis data (2.5° resolution, 6-hourly output) and a specially configured regional atmospheric model (12 km resolution, hourly output). The focus is on the month-long period in winter 2007 during the Greenland Flow Distortion Experiment. Diagnostics of upper-ocean currents and mixing are sensitive to the small-scale variability in the high-resolution regional atmospheric model. The hydrographic state of the ocean model is insensitive over the month-long experiments, however. Both sea ice and the fluxes of volume, heat, and freshwater across the east Greenland shelf break and through the Denmark Strait show a moderate response to the high-resolution atmospheric forcing. The synoptic-scale atmospheric state has a large role in controlling sea ice too, while internal ocean dynamics is the dominant factor controlling the flux diagnostics. It is the high spatial resolution, not the temporal resolution, that causes these effects, with O(10 km)-scale features being most important. The sea-level wind field is responsible, with the other atmospheric fields playing relatively minor roles. Article in Journal/Newspaper Denmark Strait East Greenland Greenland Sea ice University of East Anglia: UEA Digital Repository Greenland Quarterly Journal of the Royal Meteorological Society 135 645 2067 2085 |
institution |
Open Polar |
collection |
University of East Anglia: UEA Digital Repository |
op_collection_id |
ftuniveastangl |
language |
English |
description |
This paper quantifies and discusses the impact of high-resolution, high-frequency atmospheric forcing on the ocean circulation in the vicinity of the Denmark Strait. The approach is to force a 2 km resolution regional ocean circulation model with atmospheric states from reanalysis products that have different spatial and temporal resolutions. We use the National Center for Environmental Prediction global reanalysis data (2.5° resolution, 6-hourly output) and a specially configured regional atmospheric model (12 km resolution, hourly output). The focus is on the month-long period in winter 2007 during the Greenland Flow Distortion Experiment. Diagnostics of upper-ocean currents and mixing are sensitive to the small-scale variability in the high-resolution regional atmospheric model. The hydrographic state of the ocean model is insensitive over the month-long experiments, however. Both sea ice and the fluxes of volume, heat, and freshwater across the east Greenland shelf break and through the Denmark Strait show a moderate response to the high-resolution atmospheric forcing. The synoptic-scale atmospheric state has a large role in controlling sea ice too, while internal ocean dynamics is the dominant factor controlling the flux diagnostics. It is the high spatial resolution, not the temporal resolution, that causes these effects, with O(10 km)-scale features being most important. The sea-level wind field is responsible, with the other atmospheric fields playing relatively minor roles. |
format |
Article in Journal/Newspaper |
author |
Haine, T. W. N. Zhang, S. Moore, G. W. K. Renfrew, I. A. |
spellingShingle |
Haine, T. W. N. Zhang, S. Moore, G. W. K. Renfrew, I. A. On the impact of high-resolution, high-frequency meteorological forcing on Denmark Strait ocean circulation |
author_facet |
Haine, T. W. N. Zhang, S. Moore, G. W. K. Renfrew, I. A. |
author_sort |
Haine, T. W. N. |
title |
On the impact of high-resolution, high-frequency meteorological forcing on Denmark Strait ocean circulation |
title_short |
On the impact of high-resolution, high-frequency meteorological forcing on Denmark Strait ocean circulation |
title_full |
On the impact of high-resolution, high-frequency meteorological forcing on Denmark Strait ocean circulation |
title_fullStr |
On the impact of high-resolution, high-frequency meteorological forcing on Denmark Strait ocean circulation |
title_full_unstemmed |
On the impact of high-resolution, high-frequency meteorological forcing on Denmark Strait ocean circulation |
title_sort |
on the impact of high-resolution, high-frequency meteorological forcing on denmark strait ocean circulation |
publishDate |
2009 |
url |
https://ueaeprints.uea.ac.uk/id/eprint/24326/ https://ueaeprints.uea.ac.uk/id/eprint/24326/1/haine_etal_met_forcing_ocean_QJRMS_2009.pdf https://doi.org/10.1002/qj.505 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Denmark Strait East Greenland Greenland Sea ice |
genre_facet |
Denmark Strait East Greenland Greenland Sea ice |
op_relation |
https://ueaeprints.uea.ac.uk/id/eprint/24326/1/haine_etal_met_forcing_ocean_QJRMS_2009.pdf Haine, T. W. N., Zhang, S., Moore, G. W. K. and Renfrew, I. A. (2009) On the impact of high-resolution, high-frequency meteorological forcing on Denmark Strait ocean circulation. Quarterly Journal of the Royal Meteorological Society, 135 (645). pp. 2067-2085. ISSN 1477-870X doi:10.1002/qj.505 |
op_doi |
https://doi.org/10.1002/qj.505 |
container_title |
Quarterly Journal of the Royal Meteorological Society |
container_volume |
135 |
container_issue |
645 |
container_start_page |
2067 |
op_container_end_page |
2085 |
_version_ |
1766396602049626112 |