2002
DOI: 10.1127/0941-2948/2002/0011-0119
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Application of a radiation model for small-scale complex terrain in a GIS environment

Abstract: To calculate the radiation balance of small-scale heterogeneous terrain well known approaches were combined with the vegetation-boundary layer model HIRVAC (HIgh Resolution Vegetation Atmosphere Coupler). These modified approaches were transferred in a GIS (ArcView) environment to consider both topographic influences (terrain geometry, sky view factor) and the influence of different land uses (e.g. pasture and forest) on radiation components. The GIS application is based on the digital elevation model of the S… Show more

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Cited by 5 publications
(11 citation statements)
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“…Thus, the distributed calculation of meteorological SD-SOWA input data is primarily based on a digital elevation model (DHM/M745: Landesvermessungsamt Sachsen, 1996) with a horizontal grid size of 25 m  25 m and a vertical precision of 1 m. From the digital elevation data the values for aspect and inclination were derived for each 25 m  25 m pixel. Much of the regionalization approaches have been adapted from Goldberg and Bernhofer (2000), Goldberg andHä ntzschel (2002), andHäntzschel et al (2005). The climate effect due to the topographical situation of a single pixel is considered relative to a reference site, sufficiently close to represent the ''background climate'' of the area.…”
Section: Provision Of Spatially Distributed Meteorological Input Datamentioning
confidence: 99%
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“…Thus, the distributed calculation of meteorological SD-SOWA input data is primarily based on a digital elevation model (DHM/M745: Landesvermessungsamt Sachsen, 1996) with a horizontal grid size of 25 m  25 m and a vertical precision of 1 m. From the digital elevation data the values for aspect and inclination were derived for each 25 m  25 m pixel. Much of the regionalization approaches have been adapted from Goldberg and Bernhofer (2000), Goldberg andHä ntzschel (2002), andHäntzschel et al (2005). The climate effect due to the topographical situation of a single pixel is considered relative to a reference site, sufficiently close to represent the ''background climate'' of the area.…”
Section: Provision Of Spatially Distributed Meteorological Input Datamentioning
confidence: 99%
“…Solar radiation. Solar radiation is derived via the spatially distributed radiation model GISRAD (Goldberg and Hä ntzschel, 2002;Hä ntzschel et al, 2005) for each pixel depending on slope, aspect, and shading of the opposite slope. Main inputs are, (i) the ratio between the potential horizontal solar radiation at the reference site and the potential radiation at each pixel with a daily resolution, as well as (ii) the measured solar radiation at the reference site for each day.…”
Section: Provision Of Spatially Distributed Meteorological Input Datamentioning
confidence: 99%
“…To obtain temperature values needed for the calculation of long-wave radiation components in complex terrain the radiation model GISRAD (Goldberg & Häntzschel 2002) was linked to the coupled vegetation atmosphere model HIRVAC. HIRVAC (High Resolution Vegetation Atmosphere Coupler) is a one-and-a-half dimensional atmospheric boundary layer model (HUB), which includes a vertical high resolved vegetation canopy (based on the boundary layer model, after Mix et al 1994).…”
Section: Hirvacmentioning
confidence: 99%
“…The direct, diffuse and reflected part of the irradiance can be identified by their calculations and so the intensity of solar irradiance for each point is identifiable. The detailed equations of GISRAD are published in Goldberg (1999) and Goldberg & Häntzschel (2002).…”
Section: Extension Of the Radiation Model Gisradmentioning
confidence: 99%
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