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- 2aeb8e10-b7f8-429e-b9f6-968ece330741 definition "Blocking in the southern hemisphere typically occurs at lower latitudes when compared with the northern hemisphere. The index follows Tibaldi et al. (1994). The European blocking index is based on observations of pentad (5-day average) wind over the region 15W to 25E and 35n to 55N. If the pentad zonal wind equals the climatological value for that time period, the index is zero. If the pentad zonal wind is less than average the index is postive, while the opposite is true if the index is negative. Values close to +/- 1 indicate relatively strong events." @default.
- 2aeb8e10-b7f8-429e-b9f6-968ece330741 id "1661499" @default.
- 2aeb8e10-b7f8-429e-b9f6-968ece330741 path_id 1eb0ea0a-312c-4d74-8d42-6f1ad758f999 @default.
- 2aeb8e10-b7f8-429e-b9f6-968ece330741 path_id 23703b6b-ee15-4512-b5b2-f441547e2edf @default.
- 2aeb8e10-b7f8-429e-b9f6-968ece330741 path_id 5273c8c2-d30b-4666-b2d5-0388ce2741d0 @default.
- 2aeb8e10-b7f8-429e-b9f6-968ece330741 path_id b887d3e5-4280-43d2-a34e-0f63ac086b6a @default.
- 2aeb8e10-b7f8-429e-b9f6-968ece330741 path_id e9f67a66-e9fc-435c-b720-ae32a2c3d8f5 @default.
- 2aeb8e10-b7f8-429e-b9f6-968ece330741 path_label "ATMOSPHERIC/OCEAN INDICATORS" @default.
- 2aeb8e10-b7f8-429e-b9f6-968ece330741 path_label "CLIMATE INDICATORS" @default.
- 2aeb8e10-b7f8-429e-b9f6-968ece330741 path_label "EARTH SCIENCE" @default.
- 2aeb8e10-b7f8-429e-b9f6-968ece330741 path_label "Science Keywords" @default.
- 2aeb8e10-b7f8-429e-b9f6-968ece330741 path_label "TELECONNECTIONS" @default.
- 2aeb8e10-b7f8-429e-b9f6-968ece330741 prefLabel "BLOCKING INDEX" @default.
- 2aeb8e10-b7f8-429e-b9f6-968ece330741 reference "Tibaldi, S., E. Tosi, A. Navarra, and L. Pedulli, 1994: Northern and Southern Hemisphere seasonal variability of blocking frequency and predictability. Monthly Weather Review , 122, 1971-2003. See: http://www.cpc.noaa.gov/products/precip/CWlink/MJO/block.shtml" @default.
- 2aeb8e10-b7f8-429e-b9f6-968ece330741 tag "Science Keywords" @default.