MODIS snowline elevation changes during snowmelt runoff events in Europe
Parajka, Juraj1; Bezak, Nejc2; Burkhart, John3; Hauksson, Bjarki4; Holko, Ladislav5; Hundecha, Yeshewa6; Jenicek, Michal7; Krajci, Pavel8; Mangini, Walter9; Molnar, Peter10; Riboust, Philippe11; Rizzi, Jonathan12; Sensoy, Aynur13; Thirel, Guillaume14; Viglione, Alberto15
2019-03-01
发表期刊JOURNAL OF HYDROLOGY AND HYDROMECHANICS
ISSN0042-790X
EISSN1338-4333
卷号67期号:1页码:101-109
摘要This study evaluates MODIS snow cover characteristics for large number of snowmelt runoff events in 145 catchments from 9 countries in Europe. The analysis is based on open discharge daily time series from the Global Runoff Data Center database and daily MODIS snow cover data. Runoff events are identified by a base flow separation approach. The MODIS snow cover characteristics are derived from Terra 500 m observations (MOD10A1 dataset, V005) in the period 2000-2015 and include snow cover area, cloud coverage, regional snowline elevation (RSLE) and its changes during the snowmelt runoff events. The snowmelt events are identified by using estimated RSLE changes during a runoff event. The results indicate that in the majority of catchments there are between 3 and 6 snowmelt runoff events per year. The mean duration between the start and peak of snowmelt runoff events is about 3 days and the proportion of snowmelt events in all runoff events tends to increase with the maximum elevation of catchments. Clouds limit the estimation of snow cover area and RSLE, particularly for dates of runoff peaks. In most of the catchments, the median of cloud coverage during runoff peaks is larger than 80%. The mean minimum RSLE, which represents the conditions at the beginning of snowmelt events, is situated approximately at the mean catchment elevation. It means that snowmelt events do not start only during maximum snow cover conditions, but also after this maximum. The mean RSLE during snowmelt peaks is on average 170 m lower than at the start of the snowmelt events, but there is a large regional variability.
关键词MODIS Snowmelt Runoff events Europe Snowline elevation
DOI10.2478/johh-2018-0011
收录类别SCI
语种英语
WOS关键词Water Resources
WOS研究方向Science & Technology
WOS类目Water Resources
WOS记录号WOS:000449717800011
出版者VEDA, SLOVAK ACAD SCIENCES
引用统计
文献类型期刊论文
专题任务一_子任务一
循证社会科学证据集成
任务一
作者单位1.Vienna Univ Technol, Inst Hydraul Engn & Water Resources Management, Vienna, Austria
2.Univ Ljubljana, Fac Civil & Geodet Engn, Ljubljana, Slovenia
3.Univ Oslo, Fac Math & Nat Sci, Dept Geosci, Oslo, Norway
4.Univ Oslo, Fac Math & Nat Sci, Dept Geosci, Oslo, Norway
5.Slovak Acad Sci, Inst Hydrol, Bratislava, Slovakia
6.Swedish Meteorol & Hydrol Inst, Folkborgsvagen 17, S-60176 Norrkoping, Sweden
7.Charles Univ Prague, Dept Phys Geog & Geoecol, Prague, Czech Republic
8.Mt Rescue Serv, Avalanche Prevent Ctr, Liptovsky Hradok, Slovakia
9.Vienna Univ Technol, Inst Hydraul Engn & Water Resources Management, Vienna, Austria
10.Swiss Fed Inst Technol, Dept Civil Environm & Geomat Engn, Inst Environm Engn, Zurich, Switzerland
11.Irstea, HYCAR Res Unit HBAN, 1 Rue Pierre Gilles de Gennes,CS 10030, F-92761 Antony, France
12.UPMC Univ Paris 06, Sorbonne Univ, CNRS, EPHE,UMR 7619,Metis, 4 Pl Jussieu, F-75005 Paris, France
13.Norwegian Inst Bioecon Res, Div Forests & Forest Resources, Dept Forest & Climate, As, Norway
14.Anadolu Univ, Dept Civil Engn, Eskisehir, Turkey
15.Irstea, HYCAR Res Unit HBAN, 1 Rue Pierre Gilles de Gennes,CS 10030, F-92761 Antony, France
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GB/T 7714
Parajka, Juraj,Bezak, Nejc,Burkhart, John,et al. MODIS snowline elevation changes during snowmelt runoff events in Europe[J]. JOURNAL OF HYDROLOGY AND HYDROMECHANICS,2019,67(1):101-109.
APA Parajka, Juraj.,Bezak, Nejc.,Burkhart, John.,Hauksson, Bjarki.,Holko, Ladislav.,...&Viglione, Alberto.(2019).MODIS snowline elevation changes during snowmelt runoff events in Europe.JOURNAL OF HYDROLOGY AND HYDROMECHANICS,67(1),101-109.
MLA Parajka, Juraj,et al."MODIS snowline elevation changes during snowmelt runoff events in Europe".JOURNAL OF HYDROLOGY AND HYDROMECHANICS 67.1(2019):101-109.
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