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U.S. Geological Survey Water Supply paper, 2331. Simulation of saltwater movement in the floridan system, Hilton Head Island, South Carolina / Bush, P. W.
Titre de série : U.S. Geological Survey Water Supply paper, 2331 Titre : Simulation of saltwater movement in the floridan system, Hilton Head Island, South Carolina Type de document : texte imprimé Auteurs : Bush, P. W. Mention d'édition : U. S. Geological Survey, Federal Center Editeur : U. S. Geological Survey, Federal Center Année de publication : 1988 ISBN/ISSN/EAN : CI-05048 Note générale : The seaward hydraulic gradient that existed before pumping begain has been reserved thus increasing the potential for saltwater intrusion. Simulations of predevelopment, recent and future ground water flow in the floridan aquifer system beneath the north end of Hilton Head Island and Port Royal Sound are presented. A finite-element model for fluid-density-dependent ground water flow and solute transport was used in cross section. The general configuration of the simulated predevelopment glowfield is typical of a coastal aquifer having a seaward gradient in the freshwater. Langues : Anglais (eng) Mots-clés : Bassin HYDROGEOLOGIE Hydrogéologie Hydrologie Géologie Eau souterraine Eau salée Eau douce Simulation Index. décimale : 551.48 Hydrologie : Résumé : The seaward hydraulic gradient that existed before pumping begain has been reserved thus increasing the potential for saltwater intrusion. Simulations of predevelopment, recent and future ground water flow in the floridan aquifer system beneath the north end of Hilton Head Island and Port Royal Sound are presented. A finite-element model for fluid-density-dependent ground water flow and solute transport was used in cross section. The general configuration of the simulated predevelopment glowfield is typical of a coastal aquifer having a seaward gradient in the freshwater. Note de contenu : The seaward hydraulic gradient that existed before pumping begain has been reserved thus increasing the potential for saltwater intrusion. Simulations of predevelopment, recent and future ground water flow in the floridan aquifer system beneath the north end of Hilton Head Island and Port Royal Sound are presented. A finite-element model for fluid-density-dependent ground water flow and solute transport was used in cross section. The general configuration of the simulated predevelopment glowfield is typical of a coastal aquifer having a seaward gradient in the freshwater. U.S. Geological Survey Water Supply paper, 2331. Simulation of saltwater movement in the floridan system, Hilton Head Island, South Carolina [texte imprimé] / Bush, P. W. . - U. S. Geological Survey, Federal Center . - U. S. Geological Survey, Federal Center, 1988.
ISSN : CI-05048
The seaward hydraulic gradient that existed before pumping begain has been reserved thus increasing the potential for saltwater intrusion. Simulations of predevelopment, recent and future ground water flow in the floridan aquifer system beneath the north end of Hilton Head Island and Port Royal Sound are presented. A finite-element model for fluid-density-dependent ground water flow and solute transport was used in cross section. The general configuration of the simulated predevelopment glowfield is typical of a coastal aquifer having a seaward gradient in the freshwater.
Langues : Anglais (eng)
Mots-clés : Bassin HYDROGEOLOGIE Hydrogéologie Hydrologie Géologie Eau souterraine Eau salée Eau douce Simulation Index. décimale : 551.48 Hydrologie : Résumé : The seaward hydraulic gradient that existed before pumping begain has been reserved thus increasing the potential for saltwater intrusion. Simulations of predevelopment, recent and future ground water flow in the floridan aquifer system beneath the north end of Hilton Head Island and Port Royal Sound are presented. A finite-element model for fluid-density-dependent ground water flow and solute transport was used in cross section. The general configuration of the simulated predevelopment glowfield is typical of a coastal aquifer having a seaward gradient in the freshwater. Note de contenu : The seaward hydraulic gradient that existed before pumping begain has been reserved thus increasing the potential for saltwater intrusion. Simulations of predevelopment, recent and future ground water flow in the floridan aquifer system beneath the north end of Hilton Head Island and Port Royal Sound are presented. A finite-element model for fluid-density-dependent ground water flow and solute transport was used in cross section. The general configuration of the simulated predevelopment glowfield is typical of a coastal aquifer having a seaward gradient in the freshwater. Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B048.62608 CI-05048 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B048.62607 CI-05048 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B048.62606 CI-05048 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B048.62605 CI-05048 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B048.62604 CI-05048 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B048.62603 CI-05048 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B048.62602 CI-05048 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B048.62601 CI-05048 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible U.S. Geological survey -water supply paper, 2332. Hydrologic characteristic of the great salt lake, utach : 1847-1960 / Arnow, T.
Titre de série : U.S. Geological survey -water supply paper, 2332 Titre : Hydrologic characteristic of the great salt lake, utach : 1847-1960 Type de document : texte imprimé Auteurs : Arnow, T. ; Stephens, D. Mention d'édition : U.S. Geological survey, Federal center Editeur : U.S. Geological Survey, Federal Center Année de publication : 1990 ISBN/ISSN/EAN : CI-06006 Note générale : The great salt lake in Utah is a large of water bordered on the west by barren desert and on the east by a major metropolitan area. It is the fourth largest terminal lake in the world covering about 2, 300 square miles in 1986. Since its histoire low elevation of 4, 191.35 feet in 1986. Most of this increase (12.2 feet) occured after 1982. The rise has caused 285 millions of damage to lake side industries transportation farming, and wildlife. Accompagnying the rapid rise in lake level has been a decrease in salinity -from 28 percent in 1963 to about 6 percent in 1986. This resuted in changes in the bista of the lake from obligate haclophiles to opportupistic form such as blue-green and, most recently, a brackish fish. Langues : Anglais (eng) Mots-clés : Hydrologie Eau souterraine PRECIPITATIONS Débit solide Index. décimale : 551.48 Hydrologie : Résumé : The great salt lake in Utah is a large of water bordered on the west by barren desert and on the east by a major metropolitan area. It is the fourth largest terminal lake in the world covering about 2, 300 square miles in 1986. Since its histoire low elevation of 4, 191.35 feet in 1986. Most of this increase (12.2 feet) occured after 1982. The rise has caused 285 millions of damage to lake side industries transportation farming, and wildlife. Accompagnying the rapid rise in lake level has been a decrease in salinity -from 28 percent in 1963 to about 6 percent in 1986. This resuted in changes in the bista of the lake from obligate haclophiles to opportupistic form such as blue-green and, most recently, a brackish fish. Note de contenu : The great salt lake in Utah is a large of water bordered on the west by barren desert and on the east by a major metropolitan area. It is the fourth largest terminal lake in the world covering about 2, 300 square miles in 1986. Since its histoire low elevation of 4, 191.35 feet in 1986. Most of this increase (12.2 feet) occured after 1982. The rise has caused 285 millions of damage to lake side industries transportation farming, and wildlife. Accompagnying the rapid rise in lake level has been a decrease in salinity -from 28 percent in 1963 to about 6 percent in 1986. This resuted in changes in the bista of the lake from obligate haclophiles to opportupistic form such as blue-green and, most recently, a brackish fish. U.S. Geological survey -water supply paper, 2332. Hydrologic characteristic of the great salt lake, utach : 1847-1960 [texte imprimé] / Arnow, T. ; Stephens, D. . - U.S. Geological survey, Federal center . - U.S. Geological Survey, Federal Center, 1990.
ISSN : CI-06006
The great salt lake in Utah is a large of water bordered on the west by barren desert and on the east by a major metropolitan area. It is the fourth largest terminal lake in the world covering about 2, 300 square miles in 1986. Since its histoire low elevation of 4, 191.35 feet in 1986. Most of this increase (12.2 feet) occured after 1982. The rise has caused 285 millions of damage to lake side industries transportation farming, and wildlife. Accompagnying the rapid rise in lake level has been a decrease in salinity -from 28 percent in 1963 to about 6 percent in 1986. This resuted in changes in the bista of the lake from obligate haclophiles to opportupistic form such as blue-green and, most recently, a brackish fish.
Langues : Anglais (eng)
Mots-clés : Hydrologie Eau souterraine PRECIPITATIONS Débit solide Index. décimale : 551.48 Hydrologie : Résumé : The great salt lake in Utah is a large of water bordered on the west by barren desert and on the east by a major metropolitan area. It is the fourth largest terminal lake in the world covering about 2, 300 square miles in 1986. Since its histoire low elevation of 4, 191.35 feet in 1986. Most of this increase (12.2 feet) occured after 1982. The rise has caused 285 millions of damage to lake side industries transportation farming, and wildlife. Accompagnying the rapid rise in lake level has been a decrease in salinity -from 28 percent in 1963 to about 6 percent in 1986. This resuted in changes in the bista of the lake from obligate haclophiles to opportupistic form such as blue-green and, most recently, a brackish fish. Note de contenu : The great salt lake in Utah is a large of water bordered on the west by barren desert and on the east by a major metropolitan area. It is the fourth largest terminal lake in the world covering about 2, 300 square miles in 1986. Since its histoire low elevation of 4, 191.35 feet in 1986. Most of this increase (12.2 feet) occured after 1982. The rise has caused 285 millions of damage to lake side industries transportation farming, and wildlife. Accompagnying the rapid rise in lake level has been a decrease in salinity -from 28 percent in 1963 to about 6 percent in 1986. This resuted in changes in the bista of the lake from obligate haclophiles to opportupistic form such as blue-green and, most recently, a brackish fish. Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B006.49368 CI-06006 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B006.49367 CI-06006 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B006.49366 CI-06006 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B006.49365 CI-06006 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B006.49364 CI-06006 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B006.49363 CI-06006 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B006.49362 CI-06006 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B006.49361 CI-06006 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible U.S. Geological Survey Water Supply paper, 2333. Tritium migration from a low-level radioactive-waste disposal site near Chicago, Illinois / Nicholas, J. R.
Titre de série : U.S. Geological Survey Water Supply paper, 2333 Titre : Tritium migration from a low-level radioactive-waste disposal site near Chicago, Illinois Type de document : texte imprimé Auteurs : Nicholas, J. R. ; Healy, R. W. Mention d'édition : United States Gouvernment Printinf Office Editeur : United States Gouvernment Printinf Office Année de publication : 1988 ISBN/ISSN/EAN : CI-05060 Note générale : This paper describes the results of a study to determine the geologic and hydrologic factors that control migration of tritium from a closed, low-level radioactive-waste disposal site. The disposal site, which operated from 1943 to mid-1949, contains waste generated by research activities at the world's first nuclear reactors. Tritium has migrated horizontally at least 1,300 feet northward in glacial drift and more than 650 feet in the underlying dolomite. Thin, gently shoping sand layers in an otherwise clayey glacial drift are major conduits for ground-water flow and tritium migration in a perched zone beneath the disposal site. Tritium concentrations in the drift beneath the disposal site exceed 100,000 nanocuries per liter. Langues : Anglais (eng) Mots-clés : Géologie Hydrologie Eau de surface Eau souterraine Index. décimale : 551.48 Hydrologie : Résumé : This paper describes the results of a study to determine the geologic and hydrologic factors that control migration of tritium from a closed, low-level radioactive-waste disposal site. The disposal site, which operated from 1943 to mid-1949, contains waste generated by research activities at the world's first nuclear reactors. Tritium has migrated horizontally at least 1,300 feet northward in glacial drift and more than 650 feet in the underlying dolomite. Thin, gently shoping sand layers in an otherwise clayey glacial drift are major conduits for ground-water flow and tritium migration in a perched zone beneath the disposal site. Tritium concentrations in the drift beneath the disposal site exceed 100,000 nanocuries per liter. Note de contenu : This paper describes the results of a study to determine the geologic and hydrologic factors that control migration of tritium from a closed, low-level radioactive-waste disposal site. The disposal site, which operated from 1943 to mid-1949, contains waste generated by research activities at the world's first nuclear reactors. Tritium has migrated horizontally at least 1,300 feet northward in glacial drift and more than 650 feet in the underlying dolomite. Thin, gently shoping sand layers in an otherwise clayey glacial drift are major conduits for ground-water flow and tritium migration in a perched zone beneath the disposal site. Tritium concentrations in the drift beneath the disposal site exceed 100,000 nanocuries per liter. U.S. Geological Survey Water Supply paper, 2333. Tritium migration from a low-level radioactive-waste disposal site near Chicago, Illinois [texte imprimé] / Nicholas, J. R. ; Healy, R. W. . - United States Gouvernment Printinf Office . - United States Gouvernment Printinf Office, 1988.
ISSN : CI-05060
This paper describes the results of a study to determine the geologic and hydrologic factors that control migration of tritium from a closed, low-level radioactive-waste disposal site. The disposal site, which operated from 1943 to mid-1949, contains waste generated by research activities at the world's first nuclear reactors. Tritium has migrated horizontally at least 1,300 feet northward in glacial drift and more than 650 feet in the underlying dolomite. Thin, gently shoping sand layers in an otherwise clayey glacial drift are major conduits for ground-water flow and tritium migration in a perched zone beneath the disposal site. Tritium concentrations in the drift beneath the disposal site exceed 100,000 nanocuries per liter.
Langues : Anglais (eng)
Mots-clés : Géologie Hydrologie Eau de surface Eau souterraine Index. décimale : 551.48 Hydrologie : Résumé : This paper describes the results of a study to determine the geologic and hydrologic factors that control migration of tritium from a closed, low-level radioactive-waste disposal site. The disposal site, which operated from 1943 to mid-1949, contains waste generated by research activities at the world's first nuclear reactors. Tritium has migrated horizontally at least 1,300 feet northward in glacial drift and more than 650 feet in the underlying dolomite. Thin, gently shoping sand layers in an otherwise clayey glacial drift are major conduits for ground-water flow and tritium migration in a perched zone beneath the disposal site. Tritium concentrations in the drift beneath the disposal site exceed 100,000 nanocuries per liter. Note de contenu : This paper describes the results of a study to determine the geologic and hydrologic factors that control migration of tritium from a closed, low-level radioactive-waste disposal site. The disposal site, which operated from 1943 to mid-1949, contains waste generated by research activities at the world's first nuclear reactors. Tritium has migrated horizontally at least 1,300 feet northward in glacial drift and more than 650 feet in the underlying dolomite. Thin, gently shoping sand layers in an otherwise clayey glacial drift are major conduits for ground-water flow and tritium migration in a perched zone beneath the disposal site. Tritium concentrations in the drift beneath the disposal site exceed 100,000 nanocuries per liter. Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B060.62624 CI-05060 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B060.62623 CI-05060 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B060.62622 CI-05060 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B060.62621 CI-05060 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B060.62620 CI-05060 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B060.62619 CI-05060 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B060.62618 CI-05060 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B060.62617 CI-05060 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible U.S. Geological Survey Water Supply paper, 2335. Rainfall and runoff quantity and quality characteristics of four urban land-use catchments in Fresno, California, october 1981 to april 1983 / Altmann, R. N.
Titre de série : U.S. Geological Survey Water Supply paper, 2335 Titre : Rainfall and runoff quantity and quality characteristics of four urban land-use catchments in Fresno, California, october 1981 to april 1983 Type de document : texte imprimé Auteurs : Altmann, R. N. ; Shulters, M. V. Mention d'édition : United States Gouvernment Printing Office Editeur : United States Gouvernment Printing Office Année de publication : 1989 ISBN/ISSN/EAN : CI-05061 Note générale : Rainfall an runoff quantity and quality were monitored for industrial, single-duvelling residential, multiple-dwelling residential, and commercial land-use catchments during the 1981 - 82 and 1982 - 83 rain seasons. Storm-composite rainfall and discrete runoff samples were analysed for numerous inorganic, biological, physical and organic constituents. Atmospheric dry-deposition and street-surface particulate samples also were collected and analyzed. With the exception of the industrial catchment, the highest runoff concentrations for most constituents occurred during the initial storm runoff and then decreased throughout the remainder of the storm, independant of hydraulic conditions. Langues : Anglais (eng) Mots-clés : PRECIPITATIONS Ruissellement Urbanisme Qualité de l'eau Analyse de données Index. décimale : 551.48 Hydrologie : Résumé : Rainfall an runoff quantity and quality were monitored for industrial, single-duvelling residential, multiple-dwelling residential, and commercial land-use catchments during the 1981 - 82 and 1982 - 83 rain seasons. Storm-composite rainfall and discrete runoff samples were analysed for numerous inorganic, biological, physical and organic constituents. Atmospheric dry-deposition and street-surface particulate samples also were collected and analyzed. With the exception of the industrial catchment, the highest runoff concentrations for most constituents occurred during the initial storm runoff and then decreased throughout the remainder of the storm, independant of hydraulic conditions. Note de contenu : Rainfall an runoff quantity and quality were monitored for industrial, single-duvelling residential, multiple-dwelling residential, and commercial land-use catchments during the 1981 - 82 and 1982 - 83 rain seasons. Storm-composite rainfall and discrete runoff samples were analysed for numerous inorganic, biological, physical and organic constituents. Atmospheric dry-deposition and street-surface particulate samples also were collected and analyzed. With the exception of the industrial catchment, the highest runoff concentrations for most constituents occurred during the initial storm runoff and then decreased throughout the remainder of the storm, independant of hydraulic conditions. U.S. Geological Survey Water Supply paper, 2335. Rainfall and runoff quantity and quality characteristics of four urban land-use catchments in Fresno, California, october 1981 to april 1983 [texte imprimé] / Altmann, R. N. ; Shulters, M. V. . - United States Gouvernment Printing Office . - United States Gouvernment Printing Office, 1989.
ISSN : CI-05061
Rainfall an runoff quantity and quality were monitored for industrial, single-duvelling residential, multiple-dwelling residential, and commercial land-use catchments during the 1981 - 82 and 1982 - 83 rain seasons. Storm-composite rainfall and discrete runoff samples were analysed for numerous inorganic, biological, physical and organic constituents. Atmospheric dry-deposition and street-surface particulate samples also were collected and analyzed. With the exception of the industrial catchment, the highest runoff concentrations for most constituents occurred during the initial storm runoff and then decreased throughout the remainder of the storm, independant of hydraulic conditions.
Langues : Anglais (eng)
Mots-clés : PRECIPITATIONS Ruissellement Urbanisme Qualité de l'eau Analyse de données Index. décimale : 551.48 Hydrologie : Résumé : Rainfall an runoff quantity and quality were monitored for industrial, single-duvelling residential, multiple-dwelling residential, and commercial land-use catchments during the 1981 - 82 and 1982 - 83 rain seasons. Storm-composite rainfall and discrete runoff samples were analysed for numerous inorganic, biological, physical and organic constituents. Atmospheric dry-deposition and street-surface particulate samples also were collected and analyzed. With the exception of the industrial catchment, the highest runoff concentrations for most constituents occurred during the initial storm runoff and then decreased throughout the remainder of the storm, independant of hydraulic conditions. Note de contenu : Rainfall an runoff quantity and quality were monitored for industrial, single-duvelling residential, multiple-dwelling residential, and commercial land-use catchments during the 1981 - 82 and 1982 - 83 rain seasons. Storm-composite rainfall and discrete runoff samples were analysed for numerous inorganic, biological, physical and organic constituents. Atmospheric dry-deposition and street-surface particulate samples also were collected and analyzed. With the exception of the industrial catchment, the highest runoff concentrations for most constituents occurred during the initial storm runoff and then decreased throughout the remainder of the storm, independant of hydraulic conditions. Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B061.57080 CI-05061 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B061.57079 CI-05061 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B061.57078 CI-05061 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B061.57077 CI-05061 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B061.57076 CI-05061 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B061.57075 CI-05061 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B061.57074 CI-05061 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B061.57073 CI-05061 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible U. S. Geological Survey Water Supply paper, 2341. Floods of november 1978 to march 1979 in Arizona an west-central Neux-Mexico / Aldridge, B. N.
Titre de série : U. S. Geological Survey Water Supply paper, 2341 Titre : Floods of november 1978 to march 1979 in Arizona an west-central Neux-Mexico Type de document : texte imprimé Auteurs : Aldridge, B. N. ; Hales, T. A. Mention d'édition : U. S. Geological Survey Editeur : U. S. Geological Survey Année de publication : 1984 ISBN/ISSN/EAN : CI-05053 Note générale : Severe flooding occured in parts of the little Colorado and Gila river basins as a result of a storm that occured december 17 - 20, 1978. The central highlands received 3 to 10 inches of precipitation that was augmented by sno smelt to altitudes of 10,000 feet. The storm was preceded by entremely large amounts of rainfall and runoff in november ans was followed by other periods of high runoff in january and march 1979. In some areas flood peaks in november, january or march were higher than the peak of december 1978... Langues : Anglais (eng) Mots-clés : Météorologie Bassin versant Barrage Réservoir Inondation Hydrologie Index. décimale : 551.48 Hydrologie : Résumé : Severe flooding occured in parts of the little Colorado and Gila river basins as a result of a storm that occured december 17 - 20, 1978. The central highlands received 3 to 10 inches of precipitation that was augmented by sno smelt to altitudes of 10,000 feet. The storm was preceded by entremely large amounts of rainfall and runoff in november ans was followed by other periods of high runoff in january and march 1979. In some areas flood peaks in november, january or march were higher than the peak of december 1978... Note de contenu : Severe flooding occured in parts of the little Colorado and Gila river basins as a result of a storm that occured december 17 - 20, 1978. The central highlands received 3 to 10 inches of precipitation that was augmented by sno smelt to altitudes of 10,000 feet. The storm was preceded by entremely large amounts of rainfall and runoff in november ans was followed by other periods of high runoff in january and march 1979. In some areas flood peaks in november, january or march were higher than the peak of december 1978... U. S. Geological Survey Water Supply paper, 2341. Floods of november 1978 to march 1979 in Arizona an west-central Neux-Mexico [texte imprimé] / Aldridge, B. N. ; Hales, T. A. . - U. S. Geological Survey . - U. S. Geological Survey, 1984.
ISSN : CI-05053
Severe flooding occured in parts of the little Colorado and Gila river basins as a result of a storm that occured december 17 - 20, 1978. The central highlands received 3 to 10 inches of precipitation that was augmented by sno smelt to altitudes of 10,000 feet. The storm was preceded by entremely large amounts of rainfall and runoff in november ans was followed by other periods of high runoff in january and march 1979. In some areas flood peaks in november, january or march were higher than the peak of december 1978...
Langues : Anglais (eng)
Mots-clés : Météorologie Bassin versant Barrage Réservoir Inondation Hydrologie Index. décimale : 551.48 Hydrologie : Résumé : Severe flooding occured in parts of the little Colorado and Gila river basins as a result of a storm that occured december 17 - 20, 1978. The central highlands received 3 to 10 inches of precipitation that was augmented by sno smelt to altitudes of 10,000 feet. The storm was preceded by entremely large amounts of rainfall and runoff in november ans was followed by other periods of high runoff in january and march 1979. In some areas flood peaks in november, january or march were higher than the peak of december 1978... Note de contenu : Severe flooding occured in parts of the little Colorado and Gila river basins as a result of a storm that occured december 17 - 20, 1978. The central highlands received 3 to 10 inches of precipitation that was augmented by sno smelt to altitudes of 10,000 feet. The storm was preceded by entremely large amounts of rainfall and runoff in november ans was followed by other periods of high runoff in january and march 1979. In some areas flood peaks in november, january or march were higher than the peak of december 1978... Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B053.82210 CI-05053 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B053.82209 CI-05053 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B053.82208 CI-05053 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B053.82207 CI-05053 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B053.82206 CI-05053 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B053.82205 CI-05053 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B053.82204 CI-05053 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B053.82203 CI-05053 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible U.S. Geological survey water-supply paper, 2342. Volatilization of Benzene and eight alkyl-substituted benzene compounds from water / Rathbun, R. E.
PermalinkU.S. Geological survey water -supply paper, 2343. Evaluation of nonpotable ground water in the desert area of southeastern California for powerplant cooling / Steineman, A. C.
PermalinkU.S. Geological survey water-supply paper, 2347. Urban stormwater runoff selected background information and technics for problem assessment, with a baltimord, Maryland, case study / Fisher, G. T.
PermalinkU.S Geological Survey Water-Supply Paper, 2349. The significance of sediment transport in Arroyo development / Meyer, D.F.
PermalinkU.S. Geological Survey Water Supply paper, 2353. Geohydrology and model analysis of stream-aquifer system along the Arkansas river in Kearny an Finney countries, Southwestern Kansas / Dunlap, L. E.
PermalinkU.S Geological survey water supply paper, 2359 A. Land use, water use, streamflow characteritics and water quality characteristics of the charlotte habor inflow area, florida. / Hammett, K.M.
PermalinkU.S. Geological survey water-supply paper, 2365. Methods for estimating monthly streamflow characteristics at ungaged sites in western montana / Parret, C.
PermalinkU.S. Geological survey water-supply paper, 2366. A point-infiltration model for estimating runoff from rainfall an small basins in semiarid areas of Wyoming / Rankl, J. G.
PermalinkU.S Geological Survey Water-Supply Paper, 2371. Assessment of hydrogeologic conditions with emphasis on water quality and wastewater injection, southwest Sarasota and west Charlotte countries, Florida / Hutchinson, C.B.
PermalinkU.S geological survey water - supply paper, 2372. Methode for estimating low - flow characteristics of ungaged streams in Indiana / Arihood, L. D.
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