David M Wolock, Ph.D.
David Wolock is a Supervisory Hydrologist with the USGS Water Resources Mission Area.
Science and Products
Filter Total Items: 13
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Filter Total Items: 134
Sensitivity of water resources in the Delaware River basin to climate variability and change Sensitivity of water resources in the Delaware River basin to climate variability and change
Because of the greenhouse effect, projected increases in atmospheric carbon dioxide levels might cause global warming, which in turn could result in changes in precipitation patterns and evapotranspiration and in increases in sea level. This report describes the greenhouse effect; discusses the problems and uncertainties associated with the detection, prediction, and effects of climate...
Authors
Mark A. Ayers, David M. Wolock, Gregory J. McCabe, Lauren E. Hay, Gary D. Tasker
Sensitivity of water resources in the Delaware River basin to climate variability and change Sensitivity of water resources in the Delaware River basin to climate variability and change
Because of the "greenhouse effect," projected increases in atmospheric carbon dioxide levels might cause global warming, which in turn could result in changes in precipitation patterns and evapotranspiration and in increases in sea level. This report describes the greenhouse effect; discusses the problems and uncertainties associated with the detection, prediction, and effects of...
Authors
Mark A. Ayers, David M. Wolock, Gregory J. McCabe, Lauren E. Hay, Gary D. Tasker
Simulating the variable-source-area concept of streamflow generation with the watershed model TOPMODEL Simulating the variable-source-area concept of streamflow generation with the watershed model TOPMODEL
This report describes TOPMODEL, which is a physically based watershed model that simulates the variable-source-area concept of streamflow generation. The report describes the theoretical background, model equations, methods to determine parameter values, Fortran computer code, and an example interactive simulation. Using TOPMODEL requires specification of soils and topographic parameters
Authors
D.M. Wolock
Use of weather types to disaggregate general circulation model predictions Use of weather types to disaggregate general circulation model predictions
General circulation models (GCMs) simulate climatic conditions with a grid cell resolution on the order of 100,000 km2. This resolution is inadequate to assess the effects of climatic change on water resources at a regional scale. A method has been developed that uses weather-type analysis as a tool to spatially disaggregate GCM predictions to make them useful for water resource studies...
Authors
L.E. Hay, G. J. McCabe, D.M. Wolock, M. A. Ayers
Effects of climatic change and climatic variability on the Thornthwaite moisture index in the Delaware River basin Effects of climatic change and climatic variability on the Thornthwaite moisture index in the Delaware River basin
The Thornthwaite moisture index is useful as an indicator of the supply of water in an area relative to the demand under prevailing climatic conditions. This study examines the effects of long-term changes in climate (temperature and precipitation) on the Thornthwaite moisture index in the Delaware River basin. Temperature and precipitation estimates for doubled-CO2 conditions derived...
Authors
G. J. McCabe, D.M. Wolock
Detectability of the effects of a hypothetical temperature increase on the Thornthwaite moisture index Detectability of the effects of a hypothetical temperature increase on the Thornthwaite moisture index
Climatic changes that result from increasing concentrations of atmospheric carbon dioxide may affect the availability of water for vegetation, groundwater recharge, runoff, and human consumption. Most studies of the effects of climatic change on water resources focus on changes in mean characteristics of hydrologic variables and do not consider the effects of these changes amid natural...
Authors
G. J. McCabe, D.M. Wolock
Uncertainty in climate change and drought Uncertainty in climate change and drought
A series of projections of climate change were applied to a watershed model of the Delaware River basin to identify sources of uncertainty in predicting effects of climate change on drought in the basin as defined by New York City reservoir contents. The watershed model is a calibrated, monthly time-step water-balance model that incorporates the operation of reservoirs and diversion...
Authors
Gregory J. McCabe, David M. Wolock, Gary D. Tasker, Mark A. Ayers
Topographic effects on flow path and surface water chemistry of the Llyn Brianne catchments in Wales Topographic effects on flow path and surface water chemistry of the Llyn Brianne catchments in Wales
Topographic shape is a watershed attribute thought to influence the flow path followed by water as it traverses a catchment. Flow path, in turn, may affect the chemical composition of surface waters. Topography is quantified in the hydrological model TOPMODEL as the relative frequency distribution of the index ln(atanB), where a is the upslope area per unit contour that drains past a...
Authors
D.M. Wolock, G.M. Hornberger, T.J. Musgrove
Simulated effects of climatic change on runoff and drought in the Delaware River Basin Simulated effects of climatic change on runoff and drought in the Delaware River Basin
Various projection of climatic change were applied to watershed models of the Delaware River basin. Simulations indicate that a warming could reduce annual runoff by as much as 25 percent if current precipitation patterns continue. Simulations indicate that the largest changes in basin drought are in response to relatively small changes in precipitation. Basin drought was less sensitive...
Authors
Mark A. Ayers, Gary D. Tasker, David M. Wolock, Gregory J. McCabe, Lauren E. Hay
Effects of climatic change on the Thornthwaite moisture index Effects of climatic change on the Thornthwaite moisture index
The Thornthwaite moisture index is a useful indicator of the supply of water (precipitation) in an area relative to the demand for water under prevailing climatic conditions (potential evapotranspiration). This study examines the effects of changes in climate (temperature and precipitation) on the Thornthwaite moisture index in the conterminous United States. Estimates of changes in mean...
Authors
Gregory J. McCabe, David M. Wolock, Lauren E. Hay, Mark A. Ayers
Simulation of precipitation by weather-type analysis Simulation of precipitation by weather-type analysis
A new approach that uses weather-type analysis as a basis for stochastic precipitation modeling was developed and tested for Philadelphia, Pennsylvania. The weather types permit the identification of weather conditions associated with varying frequencies, intensities, and amounts of precipitation. Weather-type frequencies were used to stochastically simulate precipitation for...
Authors
G. J. McCabe, L.E. Hay, L.S. Kalkstein, M. A. Ayers, D.M. Wolock
Effect of climate change on watershed runoff Effect of climate change on watershed runoff
This paper examines forecasts of changes in watershed runoff in the Delaware River basin that result from a range of predicted effects of increased atmospheric carbon dioxide (CO2) on future precipitation, temperature, and stomatal resistance of plants. A deterministic hydrologic model, TOPMODEL, was driven with stochastic inputs of temperature and precipitation to derive the forecasts...
Authors
D.M. Wolock, M. A. Ayers, L.E. Hay, G. J. McCabe
Science and Products
Filter Total Items: 13
No Result Found
Filter Total Items: 134
Sensitivity of water resources in the Delaware River basin to climate variability and change Sensitivity of water resources in the Delaware River basin to climate variability and change
Because of the greenhouse effect, projected increases in atmospheric carbon dioxide levels might cause global warming, which in turn could result in changes in precipitation patterns and evapotranspiration and in increases in sea level. This report describes the greenhouse effect; discusses the problems and uncertainties associated with the detection, prediction, and effects of climate...
Authors
Mark A. Ayers, David M. Wolock, Gregory J. McCabe, Lauren E. Hay, Gary D. Tasker
Sensitivity of water resources in the Delaware River basin to climate variability and change Sensitivity of water resources in the Delaware River basin to climate variability and change
Because of the "greenhouse effect," projected increases in atmospheric carbon dioxide levels might cause global warming, which in turn could result in changes in precipitation patterns and evapotranspiration and in increases in sea level. This report describes the greenhouse effect; discusses the problems and uncertainties associated with the detection, prediction, and effects of...
Authors
Mark A. Ayers, David M. Wolock, Gregory J. McCabe, Lauren E. Hay, Gary D. Tasker
Simulating the variable-source-area concept of streamflow generation with the watershed model TOPMODEL Simulating the variable-source-area concept of streamflow generation with the watershed model TOPMODEL
This report describes TOPMODEL, which is a physically based watershed model that simulates the variable-source-area concept of streamflow generation. The report describes the theoretical background, model equations, methods to determine parameter values, Fortran computer code, and an example interactive simulation. Using TOPMODEL requires specification of soils and topographic parameters
Authors
D.M. Wolock
Use of weather types to disaggregate general circulation model predictions Use of weather types to disaggregate general circulation model predictions
General circulation models (GCMs) simulate climatic conditions with a grid cell resolution on the order of 100,000 km2. This resolution is inadequate to assess the effects of climatic change on water resources at a regional scale. A method has been developed that uses weather-type analysis as a tool to spatially disaggregate GCM predictions to make them useful for water resource studies...
Authors
L.E. Hay, G. J. McCabe, D.M. Wolock, M. A. Ayers
Effects of climatic change and climatic variability on the Thornthwaite moisture index in the Delaware River basin Effects of climatic change and climatic variability on the Thornthwaite moisture index in the Delaware River basin
The Thornthwaite moisture index is useful as an indicator of the supply of water in an area relative to the demand under prevailing climatic conditions. This study examines the effects of long-term changes in climate (temperature and precipitation) on the Thornthwaite moisture index in the Delaware River basin. Temperature and precipitation estimates for doubled-CO2 conditions derived...
Authors
G. J. McCabe, D.M. Wolock
Detectability of the effects of a hypothetical temperature increase on the Thornthwaite moisture index Detectability of the effects of a hypothetical temperature increase on the Thornthwaite moisture index
Climatic changes that result from increasing concentrations of atmospheric carbon dioxide may affect the availability of water for vegetation, groundwater recharge, runoff, and human consumption. Most studies of the effects of climatic change on water resources focus on changes in mean characteristics of hydrologic variables and do not consider the effects of these changes amid natural...
Authors
G. J. McCabe, D.M. Wolock
Uncertainty in climate change and drought Uncertainty in climate change and drought
A series of projections of climate change were applied to a watershed model of the Delaware River basin to identify sources of uncertainty in predicting effects of climate change on drought in the basin as defined by New York City reservoir contents. The watershed model is a calibrated, monthly time-step water-balance model that incorporates the operation of reservoirs and diversion...
Authors
Gregory J. McCabe, David M. Wolock, Gary D. Tasker, Mark A. Ayers
Topographic effects on flow path and surface water chemistry of the Llyn Brianne catchments in Wales Topographic effects on flow path and surface water chemistry of the Llyn Brianne catchments in Wales
Topographic shape is a watershed attribute thought to influence the flow path followed by water as it traverses a catchment. Flow path, in turn, may affect the chemical composition of surface waters. Topography is quantified in the hydrological model TOPMODEL as the relative frequency distribution of the index ln(atanB), where a is the upslope area per unit contour that drains past a...
Authors
D.M. Wolock, G.M. Hornberger, T.J. Musgrove
Simulated effects of climatic change on runoff and drought in the Delaware River Basin Simulated effects of climatic change on runoff and drought in the Delaware River Basin
Various projection of climatic change were applied to watershed models of the Delaware River basin. Simulations indicate that a warming could reduce annual runoff by as much as 25 percent if current precipitation patterns continue. Simulations indicate that the largest changes in basin drought are in response to relatively small changes in precipitation. Basin drought was less sensitive...
Authors
Mark A. Ayers, Gary D. Tasker, David M. Wolock, Gregory J. McCabe, Lauren E. Hay
Effects of climatic change on the Thornthwaite moisture index Effects of climatic change on the Thornthwaite moisture index
The Thornthwaite moisture index is a useful indicator of the supply of water (precipitation) in an area relative to the demand for water under prevailing climatic conditions (potential evapotranspiration). This study examines the effects of changes in climate (temperature and precipitation) on the Thornthwaite moisture index in the conterminous United States. Estimates of changes in mean...
Authors
Gregory J. McCabe, David M. Wolock, Lauren E. Hay, Mark A. Ayers
Simulation of precipitation by weather-type analysis Simulation of precipitation by weather-type analysis
A new approach that uses weather-type analysis as a basis for stochastic precipitation modeling was developed and tested for Philadelphia, Pennsylvania. The weather types permit the identification of weather conditions associated with varying frequencies, intensities, and amounts of precipitation. Weather-type frequencies were used to stochastically simulate precipitation for...
Authors
G. J. McCabe, L.E. Hay, L.S. Kalkstein, M. A. Ayers, D.M. Wolock
Effect of climate change on watershed runoff Effect of climate change on watershed runoff
This paper examines forecasts of changes in watershed runoff in the Delaware River basin that result from a range of predicted effects of increased atmospheric carbon dioxide (CO2) on future precipitation, temperature, and stomatal resistance of plants. A deterministic hydrologic model, TOPMODEL, was driven with stochastic inputs of temperature and precipitation to derive the forecasts...
Authors
D.M. Wolock, M. A. Ayers, L.E. Hay, G. J. McCabe