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Papers by Steve Markstrom
Fact Sheet, 2012
Given the uncertainty in climate modeling, it is desirable to use more than one GCM to obtain a r... more Given the uncertainty in climate modeling, it is desirable to use more than one GCM to obtain a range of potential future climatic conditions. Monthly precipitation and temperature output from five GCMs were processed (table 1).
Fact Sheet, 2012
Given the uncertainty in climate modeling, it is desirable to use more than one GCM to obtain a r... more Given the uncertainty in climate modeling, it is desirable to use more than one GCM to obtain a range of potential future climatic conditions. Monthly precipitation and temperature output from five GCMs were processed (table 1).
Fact Sheet, 2012
Given the uncertainty in climate modeling, it is desirable to use more than one GCM to obtain a r... more Given the uncertainty in climate modeling, it is desirable to use more than one GCM to obtain a range of potential future climatic conditions. Monthly precipitation and temperature output from five GCMs were processed (table 1).
Scientific Investigations Report, 2012
Geoscientific Model Development, 2016
This paper describes the first version of a stand-alone runoff routing tool, mizuRoute. The mizuR... more This paper describes the first version of a stand-alone runoff routing tool, mizuRoute. The mizuRoute tool post-processes runoff outputs from any distributed hydrologic model or land surface model to produce spatially distributed streamflow at various spatial scales from headwater basins to continental-wide river systems. The tool can utilize both traditional grid-based river network and vector-based river network data. Both types of river network include river segment lines and the associated drainage basin polygons, but the vector-based river network can represent finer-scale river lines than the grid-based network. Streamflow estimates at any desired location in the river network can be easily extracted from the output of mizuRoute. The routing process is simulated as two separate steps. First, hillslope routing is performed with a gamma-distribution-based unit-hydrograph to transport runoff from a hillslope to a catchment outlet. The second step is river channel routing, which i...
Scientific Investigations Report, 2015
Fact Sheet, 2012
Given the uncertainty in climate modeling, it is desirable to use more than one GCM to obtain a r... more Given the uncertainty in climate modeling, it is desirable to use more than one GCM to obtain a range of potential future climatic conditions. Monthly precipitation and temperature output from five GCMs were processed (table 1).
Fact Sheet, 2012
Given the uncertainty in climate modeling, it is desirable to use more than one GCM to obtain a r... more Given the uncertainty in climate modeling, it is desirable to use more than one GCM to obtain a range of potential future climatic conditions. Monthly precipitation and temperature output from five GCMs were processed (table 1).
Fact Sheet, 2012
Given the uncertainty in climate modeling, it is desirable to use more than one GCM to obtain a r... more Given the uncertainty in climate modeling, it is desirable to use more than one GCM to obtain a range of potential future climatic conditions. Monthly precipitation and temperature output from five GCMs were processed (table 1).
Scientific Investigations Report, 2012
Geoscientific Model Development, 2016
This paper describes the first version of a stand-alone runoff routing tool, mizuRoute. The mizuR... more This paper describes the first version of a stand-alone runoff routing tool, mizuRoute. The mizuRoute tool post-processes runoff outputs from any distributed hydrologic model or land surface model to produce spatially distributed streamflow at various spatial scales from headwater basins to continental-wide river systems. The tool can utilize both traditional grid-based river network and vector-based river network data. Both types of river network include river segment lines and the associated drainage basin polygons, but the vector-based river network can represent finer-scale river lines than the grid-based network. Streamflow estimates at any desired location in the river network can be easily extracted from the output of mizuRoute. The routing process is simulated as two separate steps. First, hillslope routing is performed with a gamma-distribution-based unit-hydrograph to transport runoff from a hillslope to a catchment outlet. The second step is river channel routing, which i...
Scientific Investigations Report, 2015