{"title":"西苏台德地区的雪水当量及其在气候变化中的变化","authors":"Grzegorz Urban","doi":"10.1016/j.ejrh.2024.101881","DOIUrl":null,"url":null,"abstract":"<div><h3>Study region</h3><p>The Western Sudetes.</p></div><div><h3>Study focus</h3><p>This paper characterises changes in snow water equivalent (SWE) in the Western Sudetes. SWE was linked to the exposure and altitude of the study area. The analysis was made for the winter seasons (November-April) 1961–2020, based on 16 measurement stations from Poland and the Czech Republic.</p><p>SWE is strongly positively correlated with snow depth (HS). The adopted method for estimating SWE (SWEi) by simple regression equations is a good and easily applicable method for climatological SWE studies. The method shows point average differences from actual SWE values in the range of 3–29 %. The overall average difference was 16.8 % and is comparable to the average difference for other mountain areas in Europe.</p></div><div><h3>New hydrological insights for the region</h3><p>The average snow depth and its SWEi gradually increase during the season, reaching maximum values in February or March, after which they decrease markedly. Meanwhile, snow density usually reaches an average monthly maximum in April. The mean and maximum seasonal SWEi values show negative trends, ranging from approximately −0.1 to −1.3 cm / decade and −0.2 to −2.5 cm / decade, respectively. These are statistically significant at many locations. SWEi values, at locations at similar altitudes, are greater at stations with a southern macro-exposure than a northern one. The rate of change of SWEi with altitude is similar on slopes with northern and southern macro-exposure. SWEi values are characterised by a positive asymmetry of differences with respect to the actual SWE. Hence, the actual SWE values are slightly smaller than the estimated values and the amount of water contributed to the environment by the snow cover decreases.</p><p>The results correspond with those from other mountainous areas in Europe, indicating decreasing SWE due to decreasing trends in snow cover thickness and duration. They are symptomatic of a warming climate, particularly intense in recent decades.</p></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":null,"pages":null},"PeriodicalIF":4.7000,"publicationDate":"2024-07-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S2214581824002301/pdfft?md5=73599d2e5dd3397f26cb7f3031ccd5c8&pid=1-s2.0-S2214581824002301-main.pdf","citationCount":"0","resultStr":"{\"title\":\"Snow water equivalent in the Western Sudetes and its changes in the light of a changing climate\",\"authors\":\"Grzegorz Urban\",\"doi\":\"10.1016/j.ejrh.2024.101881\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><h3>Study region</h3><p>The Western Sudetes.</p></div><div><h3>Study focus</h3><p>This paper characterises changes in snow water equivalent (SWE) in the Western Sudetes. SWE was linked to the exposure and altitude of the study area. The analysis was made for the winter seasons (November-April) 1961–2020, based on 16 measurement stations from Poland and the Czech Republic.</p><p>SWE is strongly positively correlated with snow depth (HS). The adopted method for estimating SWE (SWEi) by simple regression equations is a good and easily applicable method for climatological SWE studies. The method shows point average differences from actual SWE values in the range of 3–29 %. The overall average difference was 16.8 % and is comparable to the average difference for other mountain areas in Europe.</p></div><div><h3>New hydrological insights for the region</h3><p>The average snow depth and its SWEi gradually increase during the season, reaching maximum values in February or March, after which they decrease markedly. Meanwhile, snow density usually reaches an average monthly maximum in April. The mean and maximum seasonal SWEi values show negative trends, ranging from approximately −0.1 to −1.3 cm / decade and −0.2 to −2.5 cm / decade, respectively. These are statistically significant at many locations. SWEi values, at locations at similar altitudes, are greater at stations with a southern macro-exposure than a northern one. The rate of change of SWEi with altitude is similar on slopes with northern and southern macro-exposure. SWEi values are characterised by a positive asymmetry of differences with respect to the actual SWE. Hence, the actual SWE values are slightly smaller than the estimated values and the amount of water contributed to the environment by the snow cover decreases.</p><p>The results correspond with those from other mountainous areas in Europe, indicating decreasing SWE due to decreasing trends in snow cover thickness and duration. They are symptomatic of a warming climate, particularly intense in recent decades.</p></div>\",\"PeriodicalId\":48620,\"journal\":{\"name\":\"Journal of Hydrology-Regional Studies\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":4.7000,\"publicationDate\":\"2024-07-02\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://www.sciencedirect.com/science/article/pii/S2214581824002301/pdfft?md5=73599d2e5dd3397f26cb7f3031ccd5c8&pid=1-s2.0-S2214581824002301-main.pdf\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Hydrology-Regional Studies\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S2214581824002301\",\"RegionNum\":2,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"WATER RESOURCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Hydrology-Regional Studies","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S2214581824002301","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"WATER RESOURCES","Score":null,"Total":0}
Snow water equivalent in the Western Sudetes and its changes in the light of a changing climate
Study region
The Western Sudetes.
Study focus
This paper characterises changes in snow water equivalent (SWE) in the Western Sudetes. SWE was linked to the exposure and altitude of the study area. The analysis was made for the winter seasons (November-April) 1961–2020, based on 16 measurement stations from Poland and the Czech Republic.
SWE is strongly positively correlated with snow depth (HS). The adopted method for estimating SWE (SWEi) by simple regression equations is a good and easily applicable method for climatological SWE studies. The method shows point average differences from actual SWE values in the range of 3–29 %. The overall average difference was 16.8 % and is comparable to the average difference for other mountain areas in Europe.
New hydrological insights for the region
The average snow depth and its SWEi gradually increase during the season, reaching maximum values in February or March, after which they decrease markedly. Meanwhile, snow density usually reaches an average monthly maximum in April. The mean and maximum seasonal SWEi values show negative trends, ranging from approximately −0.1 to −1.3 cm / decade and −0.2 to −2.5 cm / decade, respectively. These are statistically significant at many locations. SWEi values, at locations at similar altitudes, are greater at stations with a southern macro-exposure than a northern one. The rate of change of SWEi with altitude is similar on slopes with northern and southern macro-exposure. SWEi values are characterised by a positive asymmetry of differences with respect to the actual SWE. Hence, the actual SWE values are slightly smaller than the estimated values and the amount of water contributed to the environment by the snow cover decreases.
The results correspond with those from other mountainous areas in Europe, indicating decreasing SWE due to decreasing trends in snow cover thickness and duration. They are symptomatic of a warming climate, particularly intense in recent decades.
期刊介绍:
Journal of Hydrology: Regional Studies publishes original research papers enhancing the science of hydrology and aiming at region-specific problems, past and future conditions, analysis, review and solutions. The journal particularly welcomes research papers that deliver new insights into region-specific hydrological processes and responses to changing conditions, as well as contributions that incorporate interdisciplinarity and translational science.