Downscaling of Seasonal Rainfall over the Philippines: Dynamical versus Statistical Approaches

The additional value derived from a regional climate model (RCM) nested within general circulation model (GCM) seasonal simulations, over and above statistical methods of downscaling, is compared over the Philippines for the April–June monsoon transition season. Spatial interpolation of RCM and GCM...

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Veröffentlicht in:Monthly weather review 2012-04, Vol.140 (4), p.1204-1218
Hauptverfasser: ROBERTSON, Andrew W, QIAN, Jian-Hua, TIPPETT, Michael K, MORON, Vincent, LUCERO, Anthony
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creator ROBERTSON, Andrew W
QIAN, Jian-Hua
TIPPETT, Michael K
MORON, Vincent
LUCERO, Anthony
description The additional value derived from a regional climate model (RCM) nested within general circulation model (GCM) seasonal simulations, over and above statistical methods of downscaling, is compared over the Philippines for the April–June monsoon transition season. Spatial interpolation of RCM and GCM gridbox values to station locations is compared with model output statistics (MOS) correction. The anomaly correlation coefficient (ACC) skill at the station scale of seasonal total rainfall is somewhat higher in the RCM compared to the GCM when using spatial interpolation. However, the ACC skills obtained using MOS of the GCM or RCM wind fields are shown to be generally—and rather equally—superior. The ranked probability skill scores (RPSS) are also generally much higher when using MOS, with slightly higher scores in the GCM case. Very high skills were found for MOS correction of daily rainfall frequency as a function of GCM and RCM seasonal-average low-level wind fields, but with no apparent advantage from the RCM. MOS-corrected monsoon onset dates often showed skill values similar to those of seasonal rainfall total, with good skill over the central Philippines. Finally, it is shown that the MOS skills decrease markedly and become inferior to those of spatial interpolation when the length of the 28-yr training set is halved. The results may be region dependent, and the excellent station data coverage and strong impact of ENSO on the Philippines may be factors contributing to the good MOS performance when using the full-length dataset over the Philippines.
doi_str_mv 10.1175/mwr-d-11-00177.1
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Spatial interpolation of RCM and GCM gridbox values to station locations is compared with model output statistics (MOS) correction. The anomaly correlation coefficient (ACC) skill at the station scale of seasonal total rainfall is somewhat higher in the RCM compared to the GCM when using spatial interpolation. However, the ACC skills obtained using MOS of the GCM or RCM wind fields are shown to be generally—and rather equally—superior. The ranked probability skill scores (RPSS) are also generally much higher when using MOS, with slightly higher scores in the GCM case. Very high skills were found for MOS correction of daily rainfall frequency as a function of GCM and RCM seasonal-average low-level wind fields, but with no apparent advantage from the RCM. MOS-corrected monsoon onset dates often showed skill values similar to those of seasonal rainfall total, with good skill over the central Philippines. 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source American Meteorological Society; EZB-FREE-00999 freely available EZB journals; Alma/SFX Local Collection
subjects Climate change
Climate models
Climatology
Correlation coefficient
Correlation coefficients
Daily rainfall
Datasets
Deforestation
Earth Sciences
Earth, ocean, space
El Nino
El Nino phenomena
El Nino-Southern Oscillation event
Exact sciences and technology
External geophysics
General circulation models
Interpolation
Metal oxide semiconductors
Meteorology
Monsoon onset
Monsoons
Mountains
Ocean, Atmosphere
Philippines
Precipitation
Probability theory
Rain
Rainfall
Rainfall frequency
RCM
Regional climate models
Regional climates
Sciences of the Universe
Seasonal rainfall
Seasons
Simulation
Skills
Southern Oscillation
Stations
Statistical analysis
Statistical methods
Statistics
Studies
Wind
Wind fields
title Downscaling of Seasonal Rainfall over the Philippines: Dynamical versus Statistical Approaches
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