3 rd G-VAP Workshop Fort Collins, CO September 30 – October 2, 2013 1 NOAA’s National Climatic...
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Transcript of 3 rd G-VAP Workshop Fort Collins, CO September 30 – October 2, 2013 1 NOAA’s National Climatic...
![Page 1: 3 rd G-VAP Workshop Fort Collins, CO September 30 – October 2, 2013 1 NOAA’s National Climatic Data Center Correlation of Upper Tropospheric Humidity (UTH)](https://reader030.fdocuments.net/reader030/viewer/2022032705/56649dd05503460f94ac5336/html5/thumbnails/1.jpg)
3rd G-VAP Workshop
Fort Collins, CO September 30 – October 2, 20131 NOAA’s National Climatic Data Center
Correlation of Upper Tropospheric Humidity (UTH)
with Climate IndicesLei Shi1, Carl Schreck2, Marc
Schröder3 1 NOAA/NESDIS/National Climatic Data Center, Asheville, NC, USA2 Cooperative Institute for Climate and Satellites, NC State Univ., Asheville, NC, USA3 Deutscher Wetterdienst, Satellite Based Climate Monitoring, Offenbach, Germany
![Page 2: 3 rd G-VAP Workshop Fort Collins, CO September 30 – October 2, 2013 1 NOAA’s National Climatic Data Center Correlation of Upper Tropospheric Humidity (UTH)](https://reader030.fdocuments.net/reader030/viewer/2022032705/56649dd05503460f94ac5336/html5/thumbnails/2.jpg)
3rd G-VAP Workshop
Fort Collins, CO September 30 – October 2, 20132 NOAA’s National Climatic Data Center
Datasets
• Two datasets for inter-comparison– High Resolution Infrared Radiation Sounder (HIRS)
since late 1978 (polar orbiting)– Meteosat Visible and InfraRed Imager (MVIRI) and
Spinning Enhanced Visible and InfraRed Imager (SEVIRI) since 1983 (geostationary)
![Page 3: 3 rd G-VAP Workshop Fort Collins, CO September 30 – October 2, 2013 1 NOAA’s National Climatic Data Center Correlation of Upper Tropospheric Humidity (UTH)](https://reader030.fdocuments.net/reader030/viewer/2022032705/56649dd05503460f94ac5336/html5/thumbnails/3.jpg)
3rd G-VAP Workshop
Fort Collins, CO September 30 – October 2, 20133 NOAA’s National Climatic Data Center
Climate Indices
• The value of climate indices for forecasting has been known for decades.
• A widely used one is the El Niño–Southern Oscillation (ENSO), in which persistent sea surface temperature anomalies drive distinctive weather patterns around the globe.
• Other important teleconnection patterns include the Pacific Decadal Oscillation (PDO), the Pacific–North American (PNA) pattern, the North Atlantic Oscillation (NAO), the Arctic Oscillation (AO), and the Antarctic oscillation (AAO)
• Because these patterns evolve on timescales of weeks or more, they provide critical sources of long-range predictability.
• In this assessment we compare the UTH correlation patterns to the Niño3.4, PDO, and NAO indices.
![Page 4: 3 rd G-VAP Workshop Fort Collins, CO September 30 – October 2, 2013 1 NOAA’s National Climatic Data Center Correlation of Upper Tropospheric Humidity (UTH)](https://reader030.fdocuments.net/reader030/viewer/2022032705/56649dd05503460f94ac5336/html5/thumbnails/4.jpg)
3rd G-VAP Workshop
Fort Collins, CO September 30 – October 2, 20134 NOAA’s National Climatic Data Center
Correlation with Nino 3.4 index
Source: http://www.esrl.noaa.gov/psd/enso/enso.description.html
1983 - 2009 1983 - 2009 1978 - 2011
![Page 5: 3 rd G-VAP Workshop Fort Collins, CO September 30 – October 2, 2013 1 NOAA’s National Climatic Data Center Correlation of Upper Tropospheric Humidity (UTH)](https://reader030.fdocuments.net/reader030/viewer/2022032705/56649dd05503460f94ac5336/html5/thumbnails/5.jpg)
3rd G-VAP Workshop
Fort Collins, CO September 30 – October 2, 20135 NOAA’s National Climatic Data Center
Correlation with Nino 3.4 index
Source: http://www.esrl.noaa.gov/psd/enso/enso.description.html
1983 - 2009 1978 - 2011
![Page 6: 3 rd G-VAP Workshop Fort Collins, CO September 30 – October 2, 2013 1 NOAA’s National Climatic Data Center Correlation of Upper Tropospheric Humidity (UTH)](https://reader030.fdocuments.net/reader030/viewer/2022032705/56649dd05503460f94ac5336/html5/thumbnails/6.jpg)
3rd G-VAP Workshop
Fort Collins, CO September 30 – October 2, 20136 NOAA’s National Climatic Data Center
Correlation with PDO index
1983 - 2009 1983 - 2009 1978 - 2011
![Page 7: 3 rd G-VAP Workshop Fort Collins, CO September 30 – October 2, 2013 1 NOAA’s National Climatic Data Center Correlation of Upper Tropospheric Humidity (UTH)](https://reader030.fdocuments.net/reader030/viewer/2022032705/56649dd05503460f94ac5336/html5/thumbnails/7.jpg)
3rd G-VAP Workshop
Fort Collins, CO September 30 – October 2, 20137 NOAA’s National Climatic Data Center
Correlation with PDO index
1983 - 2009 1978 - 2011
![Page 8: 3 rd G-VAP Workshop Fort Collins, CO September 30 – October 2, 2013 1 NOAA’s National Climatic Data Center Correlation of Upper Tropospheric Humidity (UTH)](https://reader030.fdocuments.net/reader030/viewer/2022032705/56649dd05503460f94ac5336/html5/thumbnails/8.jpg)
3rd G-VAP Workshop
Fort Collins, CO September 30 – October 2, 20138 NOAA’s National Climatic Data Center
Correlation with NAO index
1983 - 2009 1983 - 2009 1978 - 2011
Source: http://www.cpc.ncep.noaa.gov/data/teledoc/nao_tmap.shtml
![Page 9: 3 rd G-VAP Workshop Fort Collins, CO September 30 – October 2, 2013 1 NOAA’s National Climatic Data Center Correlation of Upper Tropospheric Humidity (UTH)](https://reader030.fdocuments.net/reader030/viewer/2022032705/56649dd05503460f94ac5336/html5/thumbnails/9.jpg)
3rd G-VAP Workshop
Fort Collins, CO September 30 – October 2, 20139 NOAA’s National Climatic Data Center
Correlation with NAO index
1983 - 2009 1978 - 2011
Source: http://www.cpc.ncep.noaa.gov/data/teledoc/nao_pmap.shtml
![Page 10: 3 rd G-VAP Workshop Fort Collins, CO September 30 – October 2, 2013 1 NOAA’s National Climatic Data Center Correlation of Upper Tropospheric Humidity (UTH)](https://reader030.fdocuments.net/reader030/viewer/2022032705/56649dd05503460f94ac5336/html5/thumbnails/10.jpg)
3rd G-VAP Workshop
Fort Collins, CO September 30 – October 2, 201310 NOAA’s National Climatic Data Center
Preliminary Findings
• Both METEOSAT UTH and HIRS UTH have high correlations with several climate indices in cold seasons
• The correlation patterns closely resemble the El Niño phase
• The correlation patterns from both datasets correspond well with the positive phases of PDO and NAO, but with some shifts in the locations of high/low index centers
• METEOSAT UTH generally has lower positive correlation values compared to those of HIRS UTH, likely due to the missing data for March 1997 through May 1998 (an El Niño event)
• METEOSAT UTH generally has higher negative correlation values compared to HIRS UTH, possibly because of overall lower UTH values in METEOSAT
• HIRS UTH has coverage for all longitudes to provide a more complete picture of the patterns