Prediction of slushflow hazard based on data from local meteorological stations.

Seeking objective criteria for slushflow prediction and warning, meteorological data has been recorded at two slushflow sites in Rana District, North Norway, during a 10 years period. The two starting zones were equipped with standard meteorological devices. In addition, the fluctuation of water lev...

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Main Authors: Bakkehøi, Steinar, Hestnes, Erik
Format: Article in Journal/Newspaper
Language:English
Published: Montana State University Library 2010
Subjects:
Online Access:https://hdl.handle.net/11250/3090620
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record_format openpolar
spelling ftngi:oai:ngi.brage.unit.no:11250/3090620 2023-10-09T21:54:16+02:00 Prediction of slushflow hazard based on data from local meteorological stations. Bakkehøi, Steinar Hestnes, Erik 2010 application/pdf https://hdl.handle.net/11250/3090620 eng eng Montana State University Library The International Snow Science Workshop (ISSW) Proceedings; https://hdl.handle.net/11250/3090620 660-663 Avalanche-RnD Snøskred-FoU Chapter 2010 ftngi 2023-09-20T22:48:33Z Seeking objective criteria for slushflow prediction and warning, meteorological data has been recorded at two slushflow sites in Rana District, North Norway, during a 10 years period. The two starting zones were equipped with standard meteorological devices. In addition, the fluctuation of water level in snowpack was monitored by pressure transmitters. The measurements were performed automatically every ten minutes. Within a distance of 20 km from the slushflow sites there are one standard climatological station and two precipitation stations. One of the main topics of the research project is to evaluate the possibility of using neighbouring meteorological stations in the prediction of current slushflow hazard and slushflow releases. Correlation of in situ measurements with records from the local meteorological stations is the basic input to the evaluation. The analysis has documented that observations at the meteorological stations can be used as a base for predicting slushflow hazard in the Rana District. The temperature and humidity are well correlated in slushflow situations while the wind speed and precipitation measurements had to be adjusted by simple models taking into account topographic characteristics, distance and elevation differences. Generally, the result indicates that slushflow prediction might be based on observations at local meteorological stations if the necessary models for parameter transformation are established. Article in Journal/Newspaper North Norway Norwegian Geotechnical Institute (NGI) Digital Archive Norway
institution Open Polar
collection Norwegian Geotechnical Institute (NGI) Digital Archive
op_collection_id ftngi
language English
topic Avalanche-RnD
Snøskred-FoU
spellingShingle Avalanche-RnD
Snøskred-FoU
Bakkehøi, Steinar
Hestnes, Erik
Prediction of slushflow hazard based on data from local meteorological stations.
topic_facet Avalanche-RnD
Snøskred-FoU
description Seeking objective criteria for slushflow prediction and warning, meteorological data has been recorded at two slushflow sites in Rana District, North Norway, during a 10 years period. The two starting zones were equipped with standard meteorological devices. In addition, the fluctuation of water level in snowpack was monitored by pressure transmitters. The measurements were performed automatically every ten minutes. Within a distance of 20 km from the slushflow sites there are one standard climatological station and two precipitation stations. One of the main topics of the research project is to evaluate the possibility of using neighbouring meteorological stations in the prediction of current slushflow hazard and slushflow releases. Correlation of in situ measurements with records from the local meteorological stations is the basic input to the evaluation. The analysis has documented that observations at the meteorological stations can be used as a base for predicting slushflow hazard in the Rana District. The temperature and humidity are well correlated in slushflow situations while the wind speed and precipitation measurements had to be adjusted by simple models taking into account topographic characteristics, distance and elevation differences. Generally, the result indicates that slushflow prediction might be based on observations at local meteorological stations if the necessary models for parameter transformation are established.
format Article in Journal/Newspaper
author Bakkehøi, Steinar
Hestnes, Erik
author_facet Bakkehøi, Steinar
Hestnes, Erik
author_sort Bakkehøi, Steinar
title Prediction of slushflow hazard based on data from local meteorological stations.
title_short Prediction of slushflow hazard based on data from local meteorological stations.
title_full Prediction of slushflow hazard based on data from local meteorological stations.
title_fullStr Prediction of slushflow hazard based on data from local meteorological stations.
title_full_unstemmed Prediction of slushflow hazard based on data from local meteorological stations.
title_sort prediction of slushflow hazard based on data from local meteorological stations.
publisher Montana State University Library
publishDate 2010
url https://hdl.handle.net/11250/3090620
geographic Norway
geographic_facet Norway
genre North Norway
genre_facet North Norway
op_source 660-663
op_relation The International Snow Science Workshop (ISSW) Proceedings;
https://hdl.handle.net/11250/3090620
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