Distributed Hydrologic Model
Intercomparison Project - Phase 2 (DMIP 2)


The Hydrology Laboratory (HL) of NOAA's National Weather Service (NWS) proposes the second phase of the Distributed Model Intercomparison Project (DMIP 2). The intent of DMIP 2 is to invite the academic community and other researchers to help guide the NOAA/NWS's distributed modeling research by participating in a comparison of distributed models applied to test data sets in two vastly different geographic regions.

DMIP 2 contains two scientific thrusts. First, we propose to continue the experiments in the DMIP 1 basins, capitalizing on nearly 4 more years of data. Additional experiments in these areas are designed as well to explore new issues not covered in DMIP 1. Second, DMIP 2 will contain experiments in two basins in the Sierra Nevada mountains, allowing researchers to test their models in areas of complex hydrology.

As in DMIP 1, HL will provide data sets for several basins. Participants will download the data sets and run their models in continuous simulation mode. Model simulations will be compared to observed streamflow data as well as simulations generated from a lumped application of the Sacramento Soil Moisture Accounting (SAC-SMA) model. Participants will be invited to meet in an HL-sponsored workshop to discuss results and future directions. Results of DMIP 2 will be used to guide future HL's distributed modeling research and applications.

We seek to identify parties interested in participating in DMIP 2 activities. To help us coordinate your participation, please provided us with information requested below. Note, both your participation in DMIP 2 and information provided below is completely voluntary. If you have questions, please contact Linchun.Wu@noaa.gov.

Organization
Point of Contact
Phone
E-mail

Level of participation:
Experiments in Oklahoma basins
Experiments in Western basins

Type of model:
Conceptual
Physical

Data needed to run your model


Parameters need to be defined or estimated. How are they derived?


Representation of hydrologic processes:
a. Spatial element over which the input is lumped


Type of snow model (if any)


b. Rainfall/runoff transformation mechanism


c. Runoff routing method within each element


d. Runoff routing method to the basin outlet


e. Method for accounting for 'sub-grid' variability of processes


Basis for specifying the resolution of the spatial element


Finest/coarsest level of resolution


Method of representing the surface/topography (e.g., TIN, grid, etc.)


Model calibration approach


What is your experience with the model?


Publications describing the model




US Dept of Commerce
National Oceanic and Atmospheric Administration
National Weather Service
Office of Climate, Water & Weather Services
1325 East West Highway
Silver Spring, MD 20910
Page Author: Linchun Wu
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Last Updated: May 31, 2013
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