Snow variability in the Swiss Alps 1864-2009

被引:51
作者
Scherrer, Simon C. [1 ]
Wuethrich, Christian [1 ,2 ]
Croci-Maspoli, Mischa [1 ]
Weingartner, Rolf [3 ]
Appenzeller, Christof [1 ]
机构
[1] Fed Off Meteorol & Climatol MeteoSwiss, Climate Div, Zurich, Switzerland
[2] Amt Umweltschutz Kanton Uri, Altdorf, Switzerland
[3] Univ Bern, Inst Geog, Grp Hydrol, CH-3012 Bern, Switzerland
关键词
new snow; snow fall; snow day; snow pack; reconstruction; climate change indicator; Switzerland; Alps; long series; decadal variability; trends; seasonal changes; INTERANNUAL VARIABILITY; CLIMATE-CHANGE; TRENDS; SCALE; COVER; INDUSTRY; DEPTH; LINKS;
D O I
10.1002/joc.3653
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
We present a climate analysis of nine unique Swiss Alpine new snow series that have been newly digitized. The stations cover different altitudes (450-1860m asl) and all time series cover more than 100years (one from 1864 to 2009). In addition, data from 71 stations for the last 50-80years for new snow and snow depth are analysed to get a more complete picture of the Swiss Alpine snow variability. Important snow climate indicators such as new snow sums (NSS), maximum new snow (MAXNS) and days with snowfall (DWSF) are calculated and variability and trends analysed. Series of days with snow pack (DWSP) 1 cm are reconstructed with useful quality for six stations using the daily new snow, local temperature and precipitation data. Our results reveal large decadal variability with phases of low and high values for NSS, DWSF and DWSP. For most stations NSS, DWSF and DWSP show the lowest values recorded and unprecedented negative trends in the late 1980s and 1990s. For MAXNS, however, no clear trends and smaller decadal variability are found but very large MAXNS values (>60cm) are missing since the year 2000. The fraction of NSS and DWSP in different seasons (autumn, winter and spring) has changed only slightly over the approximate to 150year record. Some decreases most likely attributable to temperature changes in the last 50years are found for spring, especially for NSS at low stations. Both the NSS and DWSP snow indicators show a trend reversal in most recent years (since 2000), especially at low and medium altitudes. This is consistent with the recent plateauing' (i.e. slight relative decrease) of mean winter temperature in Switzerland and illustrates how important decadal variability is in understanding the trends in key snow indicators.
引用
收藏
页码:3162 / 3173
页数:12
相关论文
共 31 条
[21]  
OECD, 2007, CLIM CHANG EUR ALPS, P136
[22]  
Peterson TC, 1998, INT J CLIMATOL, V18, P1493, DOI 10.1002/(SICI)1097-0088(19981115)18:13<1493::AID-JOC329>3.0.CO
[23]  
2-T
[24]   Trends in Swiss Alpine snow days: The role of local- and large-scale climate variability [J].
Scherrer, SC ;
Appenzeller, C ;
Laternser, M .
GEOPHYSICAL RESEARCH LETTERS, 2004, 31 (13) :L132151-4
[25]   Swiss Alpine snow pack variability: major patterns and links to local climate and large-scale flow [J].
Scherrer, Simon C. ;
Appenzeller, Christof .
CLIMATE RESEARCH, 2006, 32 (03) :187-199
[26]   Long term trend of snow depth at Sonnblick (Austrian Alps) and its relation to climate change [J].
Schoener, W. ;
Auer, I. ;
Boehm, R. .
HYDROLOGICAL PROCESSES, 2009, 23 (07) :1052-1063
[27]   Climate change and the skiing industry in southern Ontario (Canada): exploring the importance of snowmaking as a technical adaptation [J].
Scott, D ;
McBoyle, G ;
Mills, B .
CLIMATE RESEARCH, 2003, 23 (02) :171-181
[28]   Inter-annual variability and decadal trends in alpine spring phenology: A multivariate analysis approach [J].
Studer, S ;
Appenzeller, C ;
Defila, C .
CLIMATIC CHANGE, 2005, 73 (03) :395-414
[29]  
Svyashchennikov PN, 2010, 92010 MET, P32
[30]  
US Army Corps of Engineers, 1956, SNOW HYDR