Production of Temporally Consistent Gridded Precipitation and Temperature Fields for the Continental United StatesSource: Journal of Hydrometeorology:;2005:;Volume( 006 ):;issue: 003::page 330DOI: 10.1175/JHM420.1Publisher: American Meteorological Society
Abstract: The availability of long-term gridded datasets of precipitation, temperature, and other surface meteorological variables offers the potential for deriving a range of land surface conditions that have not been directly observed. These include, for instance, soil moisture, snow water equivalent, evapotranspiration, runoff, and subsurface moisture transport. However, gridding procedures can themselves introduce artificial trends due to incorporation of stations with different record lengths and locations. Hence, existing gridded datasets are in general not appropriate for estimation of long-term trends. Methods are described here for adjustment of gridded daily precipitation and temperature maxima and minima over the continental United States based on newly available (in electronic form) U.S. Cooperative Observer station data archived at the National Climatic Data Center from the early 1900s on. The intent is to produce gridded meteorological datasets that can be used, in conjunction with hydrologic modeling, for long-term trend analysis of simulated hydrologic variables.
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| contributor author | Hamlet, Alan F. | |
| contributor author | Lettenmaier, Dennis P. | |
| date accessioned | 2017-06-09T17:13:44Z | |
| date available | 2017-06-09T17:13:44Z | |
| date copyright | 2005/06/01 | |
| date issued | 2005 | |
| identifier issn | 1525-755X | |
| identifier other | ams-81427.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4224429 | |
| description abstract | The availability of long-term gridded datasets of precipitation, temperature, and other surface meteorological variables offers the potential for deriving a range of land surface conditions that have not been directly observed. These include, for instance, soil moisture, snow water equivalent, evapotranspiration, runoff, and subsurface moisture transport. However, gridding procedures can themselves introduce artificial trends due to incorporation of stations with different record lengths and locations. Hence, existing gridded datasets are in general not appropriate for estimation of long-term trends. Methods are described here for adjustment of gridded daily precipitation and temperature maxima and minima over the continental United States based on newly available (in electronic form) U.S. Cooperative Observer station data archived at the National Climatic Data Center from the early 1900s on. The intent is to produce gridded meteorological datasets that can be used, in conjunction with hydrologic modeling, for long-term trend analysis of simulated hydrologic variables. | |
| publisher | American Meteorological Society | |
| title | Production of Temporally Consistent Gridded Precipitation and Temperature Fields for the Continental United States | |
| type | Journal Paper | |
| journal volume | 6 | |
| journal issue | 3 | |
| journal title | Journal of Hydrometeorology | |
| identifier doi | 10.1175/JHM420.1 | |
| journal fristpage | 330 | |
| journal lastpage | 336 | |
| tree | Journal of Hydrometeorology:;2005:;Volume( 006 ):;issue: 003 | |
| contenttype | Fulltext |