Gregory McCabe (Former Employee)
Science and Products
Filter Total Items: 85
Variability in winter mass balance of Northern Hemisphere glaciers and relations with atmospheric circulation
An analysis of variability in the winter mass balance (WMB) of 22 glaciers in the Northern Hemisphere indicates two primary modes of variability that explain 46% of the variability among all glaciers. The first mode of variability characterizes WMB variability in Northern and Central Europe and the second mode primarily represents WMB variability in northwestern North America, but also...
Authors
G.J. McCabe, A. G. Fountain, M. Dyurgerov
Explaining spatial variability in mean annual runoff in the conterminous United States
The hydrologic concepts needed in a water-balance model to estimate the spatial variation in mean annual runoff for the 344 climate divisions in the conterminous United States (U.S.) were determined. The concepts that were evaluated were the climatic supply of water (precipitation), climatic demand for water (potential evapotranspiration), seasonality in supply and demand, and soil...
Authors
David M. Wolock, Gregory J. McCabe
Decadal variations in the strength of ENSO teleconnections with precipitation in the western United States
Changing patterns of correlations between the historical average June-November Southern Oscillation Index (SOI) and October-March precipitation totals for 84 climate divisions in the western US indicate a large amount of variability in SOI/precipitation relations on decadal time scales. Correlations of western US precipitation with SOI and other indices of tropical El Nino-Southern...
Authors
G.J. McCabe, M. D. Dettinger
Evaluating the use of “goodness‐of‐fit” measures in hydrologic and hydroclimatic model validation
Correlation and correlation‐based measures (e.g., the coefficient of determination) have been widely used to evaluate the “goodness‐of‐fit” of hydrologic and hydroclimatic models. These measures are oversensitive to extreme values (outliers) and are insensitive to additive and proportional differences between model predictions and observations. Because of these limitations, correlation...
Authors
David R. Legates, Gregory J. McCabe
A Possible connection between the 1878 yellow fever epidemic in the southern United States and the 1877-78 El Niño episode
One of the most severe outbreaks of yellow fever, a viral disease transmitted by the Aedes aegypti mosquito, affected the southern United States in the summer of 1878. The economic and human toll was enormous, and the city of Memphis, Tennessee, was one of the most affected. The authors suggest that as a consequence of one of the strongest El Niño episodes on record—that which occurred...
Authors
Henry F. Diaz, Gregory J. McCabe
General-circulation-model simulations of future snowpack in the western United States
April 1 snowpack accumulations measured at 311 snow courses in the western United States (U.S.) are grouped using a correlation-based cluster analysis. A conceptual snow accumulation and melt model and monthly temperature and precipitation for each cluster are used to estimate cluster-average April 1 snowpack. The conceptual snow model is subsequently used to estimate future snowpack by...
Authors
G.J. McCabe, D. M. Wolock
Estimates of runoff using water-balance and atmospheric general circulation models
The effects of potential climate change on mean annual runoff in the conterminous United States (U.S.) are examined using a simple water-balance model and output from two atmospheric general circulation models (GCMs). The two GCMs are from the Canadian Centre for Climate Prediction and Analysis (CCC) and the Hadley Centre for Climate Prediction and Research (HAD). In general, the CCC GCM...
Authors
D. M. Wolock, G.J. McCabe
Precipitation interpolation in mountainous regions using multiple linear regression
Multiple linear regression (MLR) was used to spatially interpolate precipitation for simulating runoff in the Animas River basin of southwestern Colorado. MLR equations were defined for each time step using measured precipitation as dependent variables. Explanatory variables used in each MLR were derived for the dependent variable locations from a digital elevation model (DEM) using a...
Authors
L. Hay, R. Viger, G. McCabe
Verification of the Rhea-orographic-precipitation model
ABSTRACT: Observed April 1 snowpack accumulations within and near the Gunnison River basin in southwestern Colorado are compared with simulations from the Rhea-orographic-precipitation model to determine if the model simulates reliable magnitudes and temporal and spatial variability in winter precipitation for the basin. Twenty simulations of the Rhea model were performed using‘optimal...
Authors
L.E. Hay, G.J. McCabe
Scale and modeling issues in water resources planning
Resource planners and managers interested in utilizing climate model output as part of their operational activities immediately confront the dilemma of scale discordance. Their functional responsibilities cover relatively small geographical areas and necessarily require data of relatively high spatial resolution. Climate models cover a large geographical, i.e. global, domain and produce...
Authors
H.F. Lins, D. M. Wolock, G.J. McCabe
Climate change and the detection of trends in annual runoff
This study examines the statistical likelihood of detecting a trend in annual runoff given an assumed change in mean annual runoff, the underlying year-to-year variability in runoff, and serial correlation of annual runoff. Means, standard deviations, and lag-1 serial correlations of annual runoff were computed for 585 stream gages in the conterminous United States, and these statistics...
Authors
G. J. McCabe, D. M. Wolock
Effects of winter atmospheric circulation on temporal and spatial variability in annual streamflow in the western United States
Winter mean 700-hectoPascal (hPa) height anomalies, representing the average atmospheric circulation during the snow season, are compared with annual streamflow measured at 140 streamgauges in the western United States. Correlation and anomaly pattern analyses are used to identify relationships between winter mean atmospheric circulation and temporal and spatial variability in annual...
Authors
G. J. McCabe
Science and Products
Filter Total Items: 85
Variability in winter mass balance of Northern Hemisphere glaciers and relations with atmospheric circulation
An analysis of variability in the winter mass balance (WMB) of 22 glaciers in the Northern Hemisphere indicates two primary modes of variability that explain 46% of the variability among all glaciers. The first mode of variability characterizes WMB variability in Northern and Central Europe and the second mode primarily represents WMB variability in northwestern North America, but also...
Authors
G.J. McCabe, A. G. Fountain, M. Dyurgerov
Explaining spatial variability in mean annual runoff in the conterminous United States
The hydrologic concepts needed in a water-balance model to estimate the spatial variation in mean annual runoff for the 344 climate divisions in the conterminous United States (U.S.) were determined. The concepts that were evaluated were the climatic supply of water (precipitation), climatic demand for water (potential evapotranspiration), seasonality in supply and demand, and soil...
Authors
David M. Wolock, Gregory J. McCabe
Decadal variations in the strength of ENSO teleconnections with precipitation in the western United States
Changing patterns of correlations between the historical average June-November Southern Oscillation Index (SOI) and October-March precipitation totals for 84 climate divisions in the western US indicate a large amount of variability in SOI/precipitation relations on decadal time scales. Correlations of western US precipitation with SOI and other indices of tropical El Nino-Southern...
Authors
G.J. McCabe, M. D. Dettinger
Evaluating the use of “goodness‐of‐fit” measures in hydrologic and hydroclimatic model validation
Correlation and correlation‐based measures (e.g., the coefficient of determination) have been widely used to evaluate the “goodness‐of‐fit” of hydrologic and hydroclimatic models. These measures are oversensitive to extreme values (outliers) and are insensitive to additive and proportional differences between model predictions and observations. Because of these limitations, correlation...
Authors
David R. Legates, Gregory J. McCabe
A Possible connection between the 1878 yellow fever epidemic in the southern United States and the 1877-78 El Niño episode
One of the most severe outbreaks of yellow fever, a viral disease transmitted by the Aedes aegypti mosquito, affected the southern United States in the summer of 1878. The economic and human toll was enormous, and the city of Memphis, Tennessee, was one of the most affected. The authors suggest that as a consequence of one of the strongest El Niño episodes on record—that which occurred...
Authors
Henry F. Diaz, Gregory J. McCabe
General-circulation-model simulations of future snowpack in the western United States
April 1 snowpack accumulations measured at 311 snow courses in the western United States (U.S.) are grouped using a correlation-based cluster analysis. A conceptual snow accumulation and melt model and monthly temperature and precipitation for each cluster are used to estimate cluster-average April 1 snowpack. The conceptual snow model is subsequently used to estimate future snowpack by...
Authors
G.J. McCabe, D. M. Wolock
Estimates of runoff using water-balance and atmospheric general circulation models
The effects of potential climate change on mean annual runoff in the conterminous United States (U.S.) are examined using a simple water-balance model and output from two atmospheric general circulation models (GCMs). The two GCMs are from the Canadian Centre for Climate Prediction and Analysis (CCC) and the Hadley Centre for Climate Prediction and Research (HAD). In general, the CCC GCM...
Authors
D. M. Wolock, G.J. McCabe
Precipitation interpolation in mountainous regions using multiple linear regression
Multiple linear regression (MLR) was used to spatially interpolate precipitation for simulating runoff in the Animas River basin of southwestern Colorado. MLR equations were defined for each time step using measured precipitation as dependent variables. Explanatory variables used in each MLR were derived for the dependent variable locations from a digital elevation model (DEM) using a...
Authors
L. Hay, R. Viger, G. McCabe
Verification of the Rhea-orographic-precipitation model
ABSTRACT: Observed April 1 snowpack accumulations within and near the Gunnison River basin in southwestern Colorado are compared with simulations from the Rhea-orographic-precipitation model to determine if the model simulates reliable magnitudes and temporal and spatial variability in winter precipitation for the basin. Twenty simulations of the Rhea model were performed using‘optimal...
Authors
L.E. Hay, G.J. McCabe
Scale and modeling issues in water resources planning
Resource planners and managers interested in utilizing climate model output as part of their operational activities immediately confront the dilemma of scale discordance. Their functional responsibilities cover relatively small geographical areas and necessarily require data of relatively high spatial resolution. Climate models cover a large geographical, i.e. global, domain and produce...
Authors
H.F. Lins, D. M. Wolock, G.J. McCabe
Climate change and the detection of trends in annual runoff
This study examines the statistical likelihood of detecting a trend in annual runoff given an assumed change in mean annual runoff, the underlying year-to-year variability in runoff, and serial correlation of annual runoff. Means, standard deviations, and lag-1 serial correlations of annual runoff were computed for 585 stream gages in the conterminous United States, and these statistics...
Authors
G. J. McCabe, D. M. Wolock
Effects of winter atmospheric circulation on temporal and spatial variability in annual streamflow in the western United States
Winter mean 700-hectoPascal (hPa) height anomalies, representing the average atmospheric circulation during the snow season, are compared with annual streamflow measured at 140 streamgauges in the western United States. Correlation and anomaly pattern analyses are used to identify relationships between winter mean atmospheric circulation and temporal and spatial variability in annual...
Authors
G. J. McCabe