A High-Resolution Lightning Map of the State of ColoradoSource: Monthly Weather Review:;2014:;volume( 142 ):;issue: 007::page 2353DOI: 10.1175/MWR-D-13-00334.1Publisher: American Meteorological Society
Abstract: or the state of Colorado, 10 years (2003?12) of 1 April?31 October cloud-to-ground (CG) lightning stroke data are mapped at 500-m spatial resolution over a 10-m spatial resolution U.S. Geological Survey (USGS) digital elevation model (DEM). Spatially, the 12.5 million strokes that are analyzed represent ground contacts, but translate to density values that are about twice the number of ground contacts. Visual interpretation of the mapped data reveals the general lightning climatology of the state, while geospatial analyses that quantify lightning activity by elevation identify certain topographic influences of Colorado?s physical landscape. Elevations lower than 1829 m (6000 ft) and above 3200 m (10 500 ft) show a positive relationship between lightning activity and elevation, while the variegated topography that lies between these two elevations is characterized by a fluctuating relationship. Though many topographic controls are elucidated through the mappings and analyses, the major finding of this paper is the sharp increase in stroke density observed above 3200 m (10 500 ft). Topography?s role in this rapid surge in stroke density, which peaks in the highest mountain summits, is not well known, and until now, was not well documented in the refereed literature at such high resolution from a long-duration dataset.
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| contributor author | Vogt, Brandon J. | |
| contributor author | Hodanish, Stephen J. | |
| date accessioned | 2017-06-09T17:31:43Z | |
| date available | 2017-06-09T17:31:43Z | |
| date copyright | 2014/07/01 | |
| date issued | 2014 | |
| identifier issn | 0027-0644 | |
| identifier other | ams-86764.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4230358 | |
| description abstract | or the state of Colorado, 10 years (2003?12) of 1 April?31 October cloud-to-ground (CG) lightning stroke data are mapped at 500-m spatial resolution over a 10-m spatial resolution U.S. Geological Survey (USGS) digital elevation model (DEM). Spatially, the 12.5 million strokes that are analyzed represent ground contacts, but translate to density values that are about twice the number of ground contacts. Visual interpretation of the mapped data reveals the general lightning climatology of the state, while geospatial analyses that quantify lightning activity by elevation identify certain topographic influences of Colorado?s physical landscape. Elevations lower than 1829 m (6000 ft) and above 3200 m (10 500 ft) show a positive relationship between lightning activity and elevation, while the variegated topography that lies between these two elevations is characterized by a fluctuating relationship. Though many topographic controls are elucidated through the mappings and analyses, the major finding of this paper is the sharp increase in stroke density observed above 3200 m (10 500 ft). Topography?s role in this rapid surge in stroke density, which peaks in the highest mountain summits, is not well known, and until now, was not well documented in the refereed literature at such high resolution from a long-duration dataset. | |
| publisher | American Meteorological Society | |
| title | A High-Resolution Lightning Map of the State of Colorado | |
| type | Journal Paper | |
| journal volume | 142 | |
| journal issue | 7 | |
| journal title | Monthly Weather Review | |
| identifier doi | 10.1175/MWR-D-13-00334.1 | |
| journal fristpage | 2353 | |
| journal lastpage | 2360 | |
| tree | Monthly Weather Review:;2014:;volume( 142 ):;issue: 007 | |
| contenttype | Fulltext |