TY - JOUR
T1 - Doubled CO2 precipitation changes for the Susquehanna basin
T2 - Down-scaling from the GENESIS general circulation model
AU - Crane, Robert G.
AU - Hewitson, Bruce C.
PY - 1998
Y1 - 1998
N2 - Artificial neural nets are used in an empirical down-scaling procedure to derive daily subgrid-scale precipitation from general circulation model (GCM) geopotential height and specific humidity data. The neural net-based transfer functions are developed using a 2° × 2.5° gridded data assimilation product from the Goddard Space Flight Center, applied to a 4 × 4 matrix of grid-cells centred on the Susquehanna river basin. The down-scaled precipitation is a close match to the observed data (temporal correlations at individual grid-points range from 0.6 to 0.84). Doubled CO2 climate change scenarios are produced by applying the same transfer functions to the geopotential height and specific humidity fields from 1 × CO2 and 2 × CO2 simulations of version II of the GENESIS climate model. The analysis indicates a 32 per cent increase in spring and summer rainfall over the basin, resulting from changes in both moisture availability and the orientation of the storm track over the region. The down-scaled precipitation increases, derived from the change in the GCM's circulation and humidity fields, are considerably larger than the change in the model's actual computed precipitation.
AB - Artificial neural nets are used in an empirical down-scaling procedure to derive daily subgrid-scale precipitation from general circulation model (GCM) geopotential height and specific humidity data. The neural net-based transfer functions are developed using a 2° × 2.5° gridded data assimilation product from the Goddard Space Flight Center, applied to a 4 × 4 matrix of grid-cells centred on the Susquehanna river basin. The down-scaled precipitation is a close match to the observed data (temporal correlations at individual grid-points range from 0.6 to 0.84). Doubled CO2 climate change scenarios are produced by applying the same transfer functions to the geopotential height and specific humidity fields from 1 × CO2 and 2 × CO2 simulations of version II of the GENESIS climate model. The analysis indicates a 32 per cent increase in spring and summer rainfall over the basin, resulting from changes in both moisture availability and the orientation of the storm track over the region. The down-scaled precipitation increases, derived from the change in the GCM's circulation and humidity fields, are considerably larger than the change in the model's actual computed precipitation.
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U2 - 10.1002/(SICI)1097-0088(199801)18:1<65::AID-JOC222>3.0.CO;2-9
DO - 10.1002/(SICI)1097-0088(199801)18:1<65::AID-JOC222>3.0.CO;2-9
M3 - Article
AN - SCOPUS:0031944625
SN - 0899-8418
VL - 18
SP - 65
EP - 76
JO - International Journal of Climatology
JF - International Journal of Climatology
IS - 1
ER -