Site Classification at the Norwegian Meteorological Institute (P3.8) Mareile Wolff, Nina Larsgård, Hildegunn Nygård, Ted Torfoss Status • Started working with the classification scheme.
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Site Classification at the Norwegian Meteorological Institute (P3.8) Mareile Wolff, Nina Larsgård, Hildegunn Nygård, Ted Torfoss Status • Started working with the classification scheme as recommended from CIMO in 2010 • Translation of the document, both as a simplified and a complete version. • Suitable tools for field measurements were considered and tested. For the present, a laser distance meter with tilt function was chosen (though not perfect). • Classification of manual precipitation stations started in 2012, ca. 20-25% of the manual precipitation stations will be classified by the end of the year. • That work will continue, eventually including the automated precipitation stations, classification for wind, temperature & humidity, and radiation. Benefits • a more objective method to characterize the exposure of a site • Improvement communication, both internal and external • possible to follow development of a station • easy to identify measures to improve the exposure of a site, also motivation • a quality measure to differentiate between stations of the Norwegian Meteorological Institute and stations of cooperation partners, see poster P3(6). • also applicable for finding new places for station Meteorologisk institutt met.no Challenges & Questions • Finding good tools which are easy to use and accurate enough (Disto not perfect) • Difficulties to judge if the natural relief is representative or not (”does a move of the station by 500m change the class obtained?”)* • How accurate is the description of natural shielding (”surrounded by obstacles of uniform height, seen under an elevation angle between 14° to 26°”)* : Class jump from 1 to 3 when surrounding trees higher than 26.5° • The shading duration due to one obstacle depends on its width and its location. That aspect is especially important for locations with high variation of sun elevation and azimuth throughout a year (high latitude countries) – – Weighting of shadowing effect by itself? Weighting of effect compared to distance of heat source/water extent • It is recommended to determine the roughness index for 30°-sectors; how to “average” the overall roughness length? 2 km? 300m? • Simplification for the actual fieldwork is needed….Schemes, diagrams, Smartphone apps, Excel sheets - What are you using? • Complete classification of an existing network will take a couple of years if no extra ”classification resources” are available • Archiving and maintaining good and usable documentation of classification results needs good planning and extra resources • Finding the right balance between improving the scheme (i.e. sector classes for wind) and overloading it • Quantifying the effect of different classes – how large is the error (Japan Mariko Kumamoto – more studies? planned studies?) Meteorologisk institutt met.no