Land surface anomaly simulations and predictions with a climate model: an El Niño Southern Oscillation case study
Author(s) -
Debbie Putt,
Keith Haines,
R. J. Gurney,
Chunlei Liu
Publication year - 2008
Publication title -
philosophical transactions of the royal society a mathematical physical and engineering sciences
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.074
H-Index - 169
eISSN - 1471-2962
pISSN - 1364-503X
DOI - 10.1098/rsta.2008.0182
Subject(s) - predictability , climatology , hadcm3 , anomaly (physics) , environmental science , data assimilation , climate model , snow , water content , atmosphere (unit) , atmospheric model , moisture , atmospheric sciences , climate change , meteorology , geology , general circulation model , gcm transcription factors , geography , oceanography , physics , geotechnical engineering , condensed matter physics , quantum mechanics
The ability of climate models to reproduce and predict land surface anomalies is an important but little-studied topic. In this study, an atmosphere and ocean assimilation scheme is used to determine whether HadCM3 can reproduce and predict snow water equivalent and soil moisture during the 1997-1998 El Niño Southern Oscillation event. Soil moisture is reproduced more successfully, though both snow and soil moisture show some predictability at 1- and 4-month lead times. This result suggests that land surface anomalies may be reasonably well initialized for climate model predictions and hydrological applications using atmospheric assimilation methods over a period of time.
Accelerating Research
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom
Address
John Eccles HouseRobert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom