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...

Full description

Bibliographic Details
Main Author: G. Levy
Format: Article
Language:English
Published: Copernicus Publications 1994-01-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/12/65/1994/angeo-12-65-1994.pdf
id doaj-7929f5b781c040d787fd736f512daed9
record_format Article
spelling 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