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U.S. Government:Supplement Au Necrologe de LAbbaie de Notre-Dame de Port-Roial Des Champs
- Livres de poche 2005, ISBN: 1234459965
[EAN: 9781234459963], Neubuch, [PU: RareBooksClub], U.S. GOVERNMENT,SUBJECTS, This item is printed on demand. Paperback. 110 pages. Original publisher: Reston, Va. : U. S. Dept. of the In… Plus…
[EAN: 9781234459963], Neubuch, [PU: RareBooksClub], U.S. GOVERNMENT,SUBJECTS, This item is printed on demand. Paperback. 110 pages. Original publisher: Reston, Va. : U. S. Dept. of the Interior, U. S. Geological Survey, 2005. OCLC Number: (OCoLC)61103773 Subject: Wildfires -- Environmental aspects -- Colorado. Excerpt: . . . 6 Analysis and Mapping of Post-Fire Hydrologic Hazards for the 2002 Wildfires Various basin and subbasin characteristics and model precipitation excess ( Soil Conservation Service, 1985 ) and was designed to account for the combined effects of unburned, parameter values are required as input to the HEC - 1 model low burn, and medium-high burn areas within a basin or sub-to compute the hydrologic processes. Basin and subbasin basin. The SCS equation for precipitation excess has the form: characteristics were derived using GIS and included drainage area, length, and slope. Model parameter values that require 2 1, 000 estimation through a model calibration process - such asP - 0. 2------------- 10RCN runoff-curve number, initial abstraction ( an adjustment ( 5 ) P --------------------------------------------------e to precipitation that describes the amount of precipitation 1, 000P 0. 8------------- 10 not expected to run off due to interception, surface-depressionRCN storage, evaporation, and other factors ), and lag time - where were defined by the equations ( Soil Conservation Service, is the precipitation excess, in inches; P 1985 ): e is the 100-year precipitation depth, in inches; P and 0. 70. 8S 1is the runoff-curve number. RCN ( 2 )-------------------------T Llag 0. 51, 900 Y For basins or subbasins that included both burned ( low, moderate, or high burn severity ) and unburned areas, the post-IA S 0. 2 ( 3 ) burn precipitation excess was computed assuming a linear-weighted combination of runoff associated with burned and unburned conditions given by: 01, 00------------S - 10 ( 4 ) !P ( P DA ) ( P DA ) ( P DA ) ( 6 ) e, subbasin e, u u e, 1 1 e, mh mh where where P is post-burn basin or subbasin precipitation is the SCS lag time; e, subb. . . This item ships from La Vergne,TN.<
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U.S. Government:Supplement Au Necrologe de LAbbaie de Notre-Dame de Port-Roial Des Champs
- Livres de poche 2005, ISBN: 9781234459963
RareBooksClub. Paperback. New. This item is printed on demand. Paperback. 110 pages. Original publisher: Reston, Va. : U. S. Dept. of the Interior, U. S. Geological Survey, 2005. OCLC N… Plus…
RareBooksClub. Paperback. New. This item is printed on demand. Paperback. 110 pages. Original publisher: Reston, Va. : U. S. Dept. of the Interior, U. S. Geological Survey, 2005. OCLC Number: (OCoLC)61103773 Subject: Wildfires -- Environmental aspects -- Colorado. Excerpt: . . . 6 Analysis and Mapping of Post-Fire Hydrologic Hazards for the 2002 Wildfires Various basin and subbasin characteristics and model precipitation excess ( Soil Conservation Service, 1985 ) and was designed to account for the combined effects of unburned, parameter values are required as input to the HEC - 1 model low burn, and medium-high burn areas within a basin or sub-to compute the hydrologic processes. Basin and subbasin basin. The SCS equation for precipitation excess has the form: characteristics were derived using GIS and included drainage area, length, and slope. Model parameter values that require 2 1, 000 estimation through a model calibration process - such asP - 0. 2------------- 10RCN runoff-curve number, initial abstraction ( an adjustment ( 5 ) P --------------------------------------------------e to precipitation that describes the amount of precipitation 1, 000P 0. 8------------- 10 not expected to run off due to interception, surface-depressionRCN storage, evaporation, and other factors ), and lag time - where were defined by the equations ( Soil Conservation Service, is the precipitation excess, in inches; P 1985 ): e is the 100-year precipitation depth, in inches; P and 0. 70. 8S 1is the runoff-curve number. RCN ( 2 )-------------------------T Llag 0. 51, 900 Y For basins or subbasins that included both burned ( low, moderate, or high burn severity ) and unburned areas, the post-IA S 0. 2 ( 3 ) burn precipitation excess was computed assuming a linear-weighted combination of runoff associated with burned and unburned conditions given by: 01, 00------------S - 10 ( 4 ) !P ( P DA ) ( P DA ) ( P DA ) ( 6 ) e, subbasin e, u u e, 1 1 e, mh mh where where P is post-burn basin or subbasin precipitation is the SCS lag time; e, subb. . . This item ships from La Vergne,TN., RareBooksClub<
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U S Government, Charles-Hugues Saint-Marc:Supplement Au Necrologe de L'Abbaie de Notre-Dame de Port-Roial Des Champs
- nouveau livre 2013, ISBN: 1234459965
[EAN: 9781234459963], Neubuch, [PU: Rarebooksclub.com], Language: eng, fre. Print On Demand.
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