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Cited by 629

The DOI matches its Crossref record; 29 of the 29 references it cites were found in a registry or an index.

A Meteorological Distribution System for High-Resolution Terrestrial Modeling (MicroMet)

Open access
Liston, Glen E., Elder, Kelly·2006·Journal of Hydrometeorology

Abstract

An intermediate-complexity, quasi–physically based, meteorological model (MicroMet) has been developed to produce high-resolution (e.g., 30-m to 1-km horizontal grid increment) atmospheric forcings required to run spatially distributed terrestrial models over a wide variety of landscapes. The following eight variables, required to run most terrestrial models, are distributed: air temperature, relative humidity, wind speed, wind direction, incoming solar radiation, incoming longwave radiation, surface pressure, and precipitation. To produce these distributions, MicroMet assumes that at least one value of each of the following meteorological variables are available for each time step, somewhere within, or near, the simulation domain: air temperature, relative humidity, wind speed, wind direction, and precipitation. These variables are collected at most meteorological stations. For the incoming solar and longwave radiation, and surface pressure, either MicroMet can use its submodels to generate these fields, or it can create the distributions from observations as part of a data assimilation procedure. MicroMet includes a preprocessor component that analyzes meteorological data, then identifies and corrects potential deficiencies. Since providing temporally and spatially continuous atmospheric forcing data for terrestrial models is a core objective of MicroMet, the preprocessor also fills in any missing data segments with realistic values. Data filling is achieved by employing a variety of procedures, including an autoregressive integrated moving average calculation for diurnally varying variables (e.g., air temperature). To create the distributed atmospheric fields, spatial interpolations are performed using the Barnes objective analysis scheme, and subsequent corrections are made to the interpolated fields using known temperature–elevation, wind–topography, humidity–cloudiness, and radiation–cloud–topography relationships.

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Metadata

Authors
Liston, G. E., & Elder, K.
Venue
Journal of Hydrometeorology
Published
2006-04-01
Volume
7
Issue
2
Pages
217-234
ISSN
  • 1525-7541 (ISSN-L)
  • 1525-755X
OpenAlex
W2162906470
Cited by
629
References
29
FWCI
9.59
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: A Meteorological Distribution System for High-Resolution Terrestrial Modeling (MicroMet). https://app.cochat.ai/papers/10.1175/jhm486.1
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Liston, G. E., & Elder, K. (2006). A Meteorological Distribution System for High-Resolution Terrestrial Modeling (MicroMet). Journal of Hydrometeorology. https://doi.org/10.1175/jhm486.1

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.