An evaluation of the National Meteorological Center weekly hindcast of upper-ocean temperature along the Eastern Pacific Equator in Junuary 1992
- California Institute of Technology, Pasadena (United States)
- National Oceanic and Atmospheric Administration, Washington, DC (United States)
The interannual El Nino warming of the surface waters of the eastern equatorial Pacific produces global atmospheric climate variations. The upper-ocean temperature distribution along the Pacific equator from 139[degrees] to 103[degrees] W was observed in January 1992 with temperature profiles recorded from a ship and inferred from an ocean general circulation model calculation involving data assimilation (i.e., hindcast). An El Nino episode was in progress. The 100-m-thick mixed layer depth, the mixed-layer temperature, and the depth-averaged temperature below the thermocline were similar in both data products. Considerable differences occurred in the representation of the 15[degrees]-25[degrees]C thermocline, such as the depth-averaged temperatures above and below the 20[degrees]C isotherm, the east-west slope of the 20[degrees]C isotherm, and a 1000-km-wide depression, The longitudinal-averaged root-mean-square difference between the hindcast and observed depths of the center of the thermocline was 17 m. Most of the disparities could be attributed to a high wavenumber transient event that the model-based assimilation system was not intended to resolve. 23 refs., 2 figs.
- OSTI ID:
- 5897038
- Journal Information:
- Journal of Climate; (United States), Vol. 6:6; ISSN 0894-8755
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
GENERAL CIRCULATION MODELS
EVALUATION
SEAS
TEMPERATURE DISTRIBUTION
SOUTHERN OSCILLATION
ANNUAL VARIATIONS
EQUATOR
MATHEMATICAL MODELS
OCEANIC CIRCULATION
PACIFIC OCEAN
SPATIAL DISTRIBUTION
DISTRIBUTION
SURFACE WATERS
VARIATIONS
540310* - Environment
Aquatic- Basic Studies- (1990-)