Southern hemisphere low level wind circulation statisticsfrom the Seasat scatterometer
Analyses of remotely sensed low-level wind vector data over the Southern Ocean are performed. Five-day averages and monthly means are created and the month-to-month variability during the winter (July-September) of 1978 is investigated. The remotely sensed winds are compared to the Australian Bu...
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Copernicus Publications
1994-01-01
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Series: | Annales Geophysicae |
Online Access: | https://www.ann-geophys.net/12/65/1994/angeo-12-65-1994.pdf |
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doaj-7929f5b781c040d787fd736f512daed92020-11-24T21:37:02ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05761994-01-0112657910.1007/s00585-994-0065-9Southern hemisphere low level wind circulation statisticsfrom the Seasat scatterometerG. LevyAnalyses of remotely sensed low-level wind vector data over the Southern Ocean are performed. Five-day averages and monthly means are created and the month-to-month variability during the winter (July-September) of 1978 is investigated. The remotely sensed winds are compared to the Australian Bureau of Meteorology (ABM) and the National Meteorological Center (NMC) surface analyses. In southern latitudes the remotely sensed winds are stronger than what the weather services' analyses suggest, indicating underestimation by ABM and NMC in these regions. The evolution of the low-level jet and the major stormtracks during the season are studied and different flow regimes are identified. The large-scale variability of the meridional flow is studied with the aid of empirical orthogonal function (EOF) analysis. The dominance of quasi-stationary wave numbers 3, 4, and 5 in the winter flow is evident in both the EOF analysis and the mean flow. The signature of an exceptionally strong blocking situation is evident in July and the special conditions leading to it are discussed. A very large intraseasonal variability with different flow regimes at different months is documented.https://www.ann-geophys.net/12/65/1994/angeo-12-65-1994.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
G. Levy |
spellingShingle |
G. Levy Southern hemisphere low level wind circulation statisticsfrom the Seasat scatterometer Annales Geophysicae |
author_facet |
G. Levy |
author_sort |
G. Levy |
title |
Southern hemisphere low level wind circulation statisticsfrom the Seasat scatterometer |
title_short |
Southern hemisphere low level wind circulation statisticsfrom the Seasat scatterometer |
title_full |
Southern hemisphere low level wind circulation statisticsfrom the Seasat scatterometer |
title_fullStr |
Southern hemisphere low level wind circulation statisticsfrom the Seasat scatterometer |
title_full_unstemmed |
Southern hemisphere low level wind circulation statisticsfrom the Seasat scatterometer |
title_sort |
southern hemisphere low level wind circulation statisticsfrom the seasat scatterometer |
publisher |
Copernicus Publications |
series |
Annales Geophysicae |
issn |
0992-7689 1432-0576 |
publishDate |
1994-01-01 |
description |
Analyses of remotely sensed low-level wind
vector data over the Southern Ocean are performed. Five-day averages and monthly
means are created and the month-to-month variability during the winter
(July-September) of 1978 is investigated. The remotely sensed winds are compared
to the Australian Bureau of Meteorology (ABM) and the National Meteorological
Center (NMC) surface analyses. In southern latitudes the remotely sensed winds
are stronger than what the weather services' analyses suggest, indicating
underestimation by ABM and NMC in these regions. The evolution of the low-level
jet and the major stormtracks during the season are studied and different flow
regimes are identified. The large-scale variability of the meridional flow is
studied with the aid of empirical orthogonal function (EOF) analysis. The
dominance of quasi-stationary wave numbers 3, 4, and 5 in the winter flow is
evident in both the EOF analysis and the mean flow. The signature of an
exceptionally strong blocking situation is evident in July and the special
conditions leading to it are discussed. A very large intraseasonal variability
with different flow regimes at different months is documented. |
url |
https://www.ann-geophys.net/12/65/1994/angeo-12-65-1994.pdf |
work_keys_str_mv |
AT glevy southernhemispherelowlevelwindcirculationstatisticsfromtheseasatscatterometer |
_version_ |
1725938695082606592 |