M. Aniya, Alejandro Dusaillant, J. O'kuinghttons, G. Barcaza, Sidi Bravo
{"title":"拉古纳德洛斯特姆帕诺斯,斯特芬冰川侧湖,海洛Patagónico北,智利,自1974年","authors":"M. Aniya, Alejandro Dusaillant, J. O'kuinghttons, G. Barcaza, Sidi Bravo","doi":"10.5331/bgr.20r01","DOIUrl":null,"url":null,"abstract":"Glacier lake outburst floods (GLOF) at Laguna de los Témpanos, a glacier-dammed side lake of Glaciar Steffen, Hielo Patagónico Norte, were documented for a period between December 1974 and February 2020. With manual interpretation of 150 remote sensing images of aerial surveys, vertical aerial photographs, Landsat MSS, TM, ETM and OLI, ALOS, and ASTER images, 19 GLOFs were captured/inferred by focusing on icebergs and water levels, except two periods in the 1980 s and the 1990 s for which no image was available. This translates to the occurrence of the GLOF on average once ca. every 14 months. Many GLOFs occurred in late summer to early fall, with a few in late spring: but one GLOF was inferred to have occurred in wintertime. The causes of GLOFs were supposed to be heavy rainfalls, probably accompanied with rapid snow/ice melting by warm air temperatures, judging from the general weather condition over the laguna area. The latest two GLOFs (2016 & 2017) were very large, enough to have completely exposed the lake floor in the middle section. The GLOF of 2017 (Mar. 31) was registered in a hydrograph set up at Lower Río Huemules. After this GLOF, the water level has become stable with a more or less continuous outlet stream along the glacier sidewall and there has been no GLOF to date. So probably the prospect of another GLOF has considerably diminished by now. As Glaciar Steffen receded about 6 km during this study period, the glacier has thinned accordingly, to which the water level adjusted with three distinctive relatively stable states while fluctuating frequently.","PeriodicalId":9345,"journal":{"name":"Bulletin of glaciological research","volume":null,"pages":null},"PeriodicalIF":1.0000,"publicationDate":"2020-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":"{\"title\":\"GLOFs of Laguna de los Témpanos, glacier-dammed side lake of Glaciar Steffen, Hielo Patagónico Norte, Chile, since 1974\",\"authors\":\"M. Aniya, Alejandro Dusaillant, J. O'kuinghttons, G. Barcaza, Sidi Bravo\",\"doi\":\"10.5331/bgr.20r01\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Glacier lake outburst floods (GLOF) at Laguna de los Témpanos, a glacier-dammed side lake of Glaciar Steffen, Hielo Patagónico Norte, were documented for a period between December 1974 and February 2020. With manual interpretation of 150 remote sensing images of aerial surveys, vertical aerial photographs, Landsat MSS, TM, ETM and OLI, ALOS, and ASTER images, 19 GLOFs were captured/inferred by focusing on icebergs and water levels, except two periods in the 1980 s and the 1990 s for which no image was available. This translates to the occurrence of the GLOF on average once ca. every 14 months. Many GLOFs occurred in late summer to early fall, with a few in late spring: but one GLOF was inferred to have occurred in wintertime. The causes of GLOFs were supposed to be heavy rainfalls, probably accompanied with rapid snow/ice melting by warm air temperatures, judging from the general weather condition over the laguna area. The latest two GLOFs (2016 & 2017) were very large, enough to have completely exposed the lake floor in the middle section. The GLOF of 2017 (Mar. 31) was registered in a hydrograph set up at Lower Río Huemules. After this GLOF, the water level has become stable with a more or less continuous outlet stream along the glacier sidewall and there has been no GLOF to date. So probably the prospect of another GLOF has considerably diminished by now. As Glaciar Steffen receded about 6 km during this study period, the glacier has thinned accordingly, to which the water level adjusted with three distinctive relatively stable states while fluctuating frequently.\",\"PeriodicalId\":9345,\"journal\":{\"name\":\"Bulletin of glaciological research\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":1.0000,\"publicationDate\":\"2020-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"2\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Bulletin of glaciological research\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.5331/bgr.20r01\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"GEOGRAPHY, PHYSICAL\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Bulletin of glaciological research","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5331/bgr.20r01","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"GEOGRAPHY, PHYSICAL","Score":null,"Total":0}
引用次数: 2
摘要
1974年12月至2020年2月期间,研究人员记录了拉古纳德洛斯特姆帕诺斯冰川湖爆发洪水(GLOF),拉古纳德洛斯特姆帕诺斯冰川湖是位于Patagónico北部的斯特芬冰川的一个冰川大坝侧湖。通过人工解译150幅遥感图像,包括航空调查、垂直航空照片、Landsat MSS、TM、ETM和OLI、ALOS和ASTER图像,除了20世纪80年代和90年代两个没有图像的时期外,通过聚焦冰山和水位捕获/推断出了19幅GLOFs。这意味着GLOF平均每14个月发生一次。许多GLOF发生在夏末至初秋,少数发生在晚春,但据推测,有一次GLOF发生在冬季。从拉古纳地区的一般天气状况来看,GLOFs的原因应该是暴雨,可能伴随着温暖的空气温度导致的冰雪快速融化。最近的两次GLOFs(2016年和2017年)非常大,足以完全暴露中段的湖底。2017年(3月31日)的GLOF在Lower Río Huemules设立的水道中注册。此后,水位趋于稳定,沿冰川侧壁有一条或多或少连续的出水口流,迄今为止没有发生过GLOF。因此,到目前为止,另一次全球大萧条的前景可能已经大大减弱。随着Steffen冰川在本研究期间后退约6 km,冰川随之变薄,水位在频繁波动的同时以三种不同的相对稳定状态进行调整。
GLOFs of Laguna de los Témpanos, glacier-dammed side lake of Glaciar Steffen, Hielo Patagónico Norte, Chile, since 1974
Glacier lake outburst floods (GLOF) at Laguna de los Témpanos, a glacier-dammed side lake of Glaciar Steffen, Hielo Patagónico Norte, were documented for a period between December 1974 and February 2020. With manual interpretation of 150 remote sensing images of aerial surveys, vertical aerial photographs, Landsat MSS, TM, ETM and OLI, ALOS, and ASTER images, 19 GLOFs were captured/inferred by focusing on icebergs and water levels, except two periods in the 1980 s and the 1990 s for which no image was available. This translates to the occurrence of the GLOF on average once ca. every 14 months. Many GLOFs occurred in late summer to early fall, with a few in late spring: but one GLOF was inferred to have occurred in wintertime. The causes of GLOFs were supposed to be heavy rainfalls, probably accompanied with rapid snow/ice melting by warm air temperatures, judging from the general weather condition over the laguna area. The latest two GLOFs (2016 & 2017) were very large, enough to have completely exposed the lake floor in the middle section. The GLOF of 2017 (Mar. 31) was registered in a hydrograph set up at Lower Río Huemules. After this GLOF, the water level has become stable with a more or less continuous outlet stream along the glacier sidewall and there has been no GLOF to date. So probably the prospect of another GLOF has considerably diminished by now. As Glaciar Steffen receded about 6 km during this study period, the glacier has thinned accordingly, to which the water level adjusted with three distinctive relatively stable states while fluctuating frequently.