A New Teleconnection : The Australian Southern Oscillation

A possibly new teleconnection has been discovered off the east coast of Australia in the region around Tasman sea and Southern Ocean. Found in pressure anomalies using a novel graph based approach called shared reciprocal nearest neighbors, this dipole appears in reanalysis datasets such as NCEP, JR...

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Main Authors: Kumar, Arjun, Liess, Stefan, Kawale, Jaya, Ormsby, Dominick, Steinhaeuser, Karsten, Kumar, Vipin
Format: Report
Language:English
Published: 2012
Subjects:
Online Access:http://hdl.handle.net/11299/215898
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record_format openpolar
spelling ftunivminnesdc:oai:conservancy.umn.edu:11299/215898 2023-05-15T13:57:08+02:00 A New Teleconnection : The Australian Southern Oscillation Kumar, Arjun Liess, Stefan Kawale, Jaya Ormsby, Dominick Steinhaeuser, Karsten Kumar, Vipin 2012-09-21 http://hdl.handle.net/11299/215898 en_US eng Technical Report; 12-020 http://hdl.handle.net/11299/215898 Report 2012 ftunivminnesdc 2020-09-04T13:43:44Z A possibly new teleconnection has been discovered off the east coast of Australia in the region around Tasman sea and Southern Ocean. Found in pressure anomalies using a novel graph based approach called shared reciprocal nearest neighbors, this dipole appears in reanalysis datasets such as NCEP, JRA, ERA and MERRA. The HadSLP2 observation data shows the new dipole, despite of limited observations in the Tasman Sea. Tests are performed in order to understand the uniqueness of the dipole and its relationship to existing well known phenomena. The dipole index is correlated with known dipole indices such as the SO (Southern Oscillation), AAO (Antarctic Oscillation) with which it shares a marginally higher correlation of less than 0.4 and other northern teleconnections with which it is shown to have a poor relationship. We limit further analysis with only the AAO and SO indices as these are spatially close, have a higher correlation with the new index and tend to influence it in one or more seasons. Seasonal analysis is done to look at the variation in strength as well as its influence on other variables such as TAS (Temperature at Surface), OLR (Outgoing Longwave Radiation), Precipitation etc. We also look at composite maps and do significance tests to determine the significant regions in these maps. We also determine regions that are influenced by the new dipole index alone and are not influenced by other dipoles namely the SO and AAO by looking at difference maps. We discover the dipole at different geopotential heights - 700 hPa, 500 hPa and 50 hPa (Sea Level Pressure is 1013 hPa)- and determine if the dipole is a sea surface phenomenon such as the SO or an upper atmospheric phenomenon such as the AAO. Our tests have shown that we may indeed be looking at a new phenomenon and further tests are being conducted to confirm that. Report Antarc* Antarctic Southern Ocean University of Minnesota Digital Conservancy Antarctic Merra ENVELOPE(12.615,12.615,65.816,65.816) Southern Ocean
institution Open Polar
collection University of Minnesota Digital Conservancy
op_collection_id ftunivminnesdc
language English
description A possibly new teleconnection has been discovered off the east coast of Australia in the region around Tasman sea and Southern Ocean. Found in pressure anomalies using a novel graph based approach called shared reciprocal nearest neighbors, this dipole appears in reanalysis datasets such as NCEP, JRA, ERA and MERRA. The HadSLP2 observation data shows the new dipole, despite of limited observations in the Tasman Sea. Tests are performed in order to understand the uniqueness of the dipole and its relationship to existing well known phenomena. The dipole index is correlated with known dipole indices such as the SO (Southern Oscillation), AAO (Antarctic Oscillation) with which it shares a marginally higher correlation of less than 0.4 and other northern teleconnections with which it is shown to have a poor relationship. We limit further analysis with only the AAO and SO indices as these are spatially close, have a higher correlation with the new index and tend to influence it in one or more seasons. Seasonal analysis is done to look at the variation in strength as well as its influence on other variables such as TAS (Temperature at Surface), OLR (Outgoing Longwave Radiation), Precipitation etc. We also look at composite maps and do significance tests to determine the significant regions in these maps. We also determine regions that are influenced by the new dipole index alone and are not influenced by other dipoles namely the SO and AAO by looking at difference maps. We discover the dipole at different geopotential heights - 700 hPa, 500 hPa and 50 hPa (Sea Level Pressure is 1013 hPa)- and determine if the dipole is a sea surface phenomenon such as the SO or an upper atmospheric phenomenon such as the AAO. Our tests have shown that we may indeed be looking at a new phenomenon and further tests are being conducted to confirm that.
format Report
author Kumar, Arjun
Liess, Stefan
Kawale, Jaya
Ormsby, Dominick
Steinhaeuser, Karsten
Kumar, Vipin
spellingShingle Kumar, Arjun
Liess, Stefan
Kawale, Jaya
Ormsby, Dominick
Steinhaeuser, Karsten
Kumar, Vipin
A New Teleconnection : The Australian Southern Oscillation
author_facet Kumar, Arjun
Liess, Stefan
Kawale, Jaya
Ormsby, Dominick
Steinhaeuser, Karsten
Kumar, Vipin
author_sort Kumar, Arjun
title A New Teleconnection : The Australian Southern Oscillation
title_short A New Teleconnection : The Australian Southern Oscillation
title_full A New Teleconnection : The Australian Southern Oscillation
title_fullStr A New Teleconnection : The Australian Southern Oscillation
title_full_unstemmed A New Teleconnection : The Australian Southern Oscillation
title_sort new teleconnection : the australian southern oscillation
publishDate 2012
url http://hdl.handle.net/11299/215898
long_lat ENVELOPE(12.615,12.615,65.816,65.816)
geographic Antarctic
Merra
Southern Ocean
geographic_facet Antarctic
Merra
Southern Ocean
genre Antarc*
Antarctic
Southern Ocean
genre_facet Antarc*
Antarctic
Southern Ocean
op_relation Technical Report; 12-020
http://hdl.handle.net/11299/215898
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