Project Summary

Download MT-CLIM 4.3

Meteorology at the land surface affects many processes in the terrestrial biogeochemical system. Measurements of near-surface meteorological conditions are made at many locations, but we are often faced with having to perform ecosystem process simulations in areas where no meteorological measurements have been taken. In some cases it is possible to install new instrumentation for a particular study, but there are many situations where this is not a feasible solution. We developed MT-CLIM to address the problems of estimating daily near-surface meteorological parameters from nearby observations. It is designed to handle the special problems encountered in mountainous terrain, but it is applicable in flat terrain as well.


MT-CLIM is a computer program that uses observations of daily maximum temperature, minimum temperature, and precipitation from one location (the "base") to estimate the temperature, precipitation, radiation, and humidity at another location (the "site"). The base and the site can be at different elevations, and can have different slopes and aspects. Better results are obtained when the base and site are relatively close to one another (at the bottom and the top of a valley, for example).

Temperature estimates at the site are based on the base temperatures and a user-supplied temperature lapse rate. Separate lapse rates can be supplied for daily maximum and minimum temperature. Precipitation estimates at the site are based on the daily record of preciupitation from the base, and a user-specified ratio of annual total precipitation between the site and the base.

The estimation of radiation and humidity are more complex, since these parameters are not assumed to be measured at the base station. Humidity estimates are based on the observation that daily minimum temperature is usually very close to dewpoint temperature. The MT-CLIM algorithm includes corrections to this assumption for arid climates. Radiation estimates are based on the observation that the diurnal temperature range (from minimum temperature to maximum temperature) is closely related to the daily average atmospheric transmittance. In conjunction with information about the latitude, elevation, slope, and aspect of the site, this relationship can be used to estimate daily total radiation with a typical error range of +/- 15%. Some of the limitations of MT-CLIM are the use of a single base station for observations and the need for the user to specify the temperature and precipitation relationships with elevation. We have developed an expanded version of the MT-CLIM logic, called Daymet, that uses observations from a large number of base stations.

Mountain Climate Simulator


Bristow, K.L., and G.S. Campbell, 1984. On the relationship between incoming solar radiation and daily maximum and minimum temperature. Agricultural and Forest Meteorology, 31:159-166.

Running, S.W., R.R. Nemani, and R.D. Hungerford, 1987. Extrapolation of synoptic meteorological data in mountainous terrain and its use for simulating forest evaporation and photosynthesis. Canadian Journal of Forest Research, 17:472-483.

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