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Design of climate station network in mountain catchments
by
Punčochář, Petr
, Křeček, Josef
in
Air temperature
/ Catchments
/ Climate
/ climate station network
/ Density
/ Hypsometry
/ Meteorological data
/ mountain watershed
/ Mountains
/ potential evapotranspiration
/ precipitation
/ Root-mean-square errors
/ Spatial data
/ spatial data interpolation
/ Watershed management
/ Wind speed
2012
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Design of climate station network in mountain catchments
by
Punčochář, Petr
, Křeček, Josef
in
Air temperature
/ Catchments
/ Climate
/ climate station network
/ Density
/ Hypsometry
/ Meteorological data
/ mountain watershed
/ Mountains
/ potential evapotranspiration
/ precipitation
/ Root-mean-square errors
/ Spatial data
/ spatial data interpolation
/ Watershed management
/ Wind speed
2012
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While trying to remove the title from your shelf something went wrong :( Kindly try again later!
Do you wish to request the book?
Design of climate station network in mountain catchments
by
Punčochář, Petr
, Křeček, Josef
in
Air temperature
/ Catchments
/ Climate
/ climate station network
/ Density
/ Hypsometry
/ Meteorological data
/ mountain watershed
/ Mountains
/ potential evapotranspiration
/ precipitation
/ Root-mean-square errors
/ Spatial data
/ spatial data interpolation
/ Watershed management
/ Wind speed
2012
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Journal Article
Design of climate station network in mountain catchments
2012
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Overview
In the Jizera Mountains (Czech Republic) the density of climate station network was tested in relation to spatial data interpolation, and watershed management targets. Point weather data (precipitation, air temperature, humidity and wind velocity) were interpolated by the nearest neighbourhood (NN), inverse distance weighting (IDW), spline (SPL), hypsometric (HYP) and kriging (KRI) methods. The results were assessed by the root mean square error (RMSE). The interpolation effectiveness showed the following order: HYP, IDW, KRI, NN and SPL. The advantage of the hypsometric method was recognised, particularly, by providing reasonable outputs in marginal catchments of the region and outside of the main instrumented area. However, in case of a higher density of observation points (11 hectares per station), all interpolation methods manifested comparable and realistic outputs in the focused mountain watersheds.
Publisher
Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Geographical Institute,Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences
Subject
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