DOI: | 10.1002/2015GL065321
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论文题名: | Measuring glacier surface temperatures with ground-based thermal infrared imaging |
作者: | Aubry-Wake C.; Baraer M.; McKenzie J.M.; Mark B.G.; Wigmore O.; Hellström R.Å.; Lautz L.; Somers L.
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刊名: | Geophysical Research Letters
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ISSN: | 0094-9292
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EISSN: | 1944-9023
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出版年: | 2015
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卷: | 42, 期:20 | 起始页码: | 8489
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结束页码: | 8497
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语种: | 英语
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英文关键词: | energy budget
; glacier
; infrared camera
; Peru
; temperature
; Thermal imagery
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Scopus关键词: | Atmospheric temperature
; Budget control
; Cameras
; Correlation methods
; Glaciers
; Infrared devices
; Infrared radiation
; Meteorology
; Spatial distribution
; Surface properties
; Temperature
; Temperature indicating cameras
; Thermography (imaging)
; Energy budgets
; Infra-red cameras
; Pearson's correlation coefficients
; Peru
; Surface temperatures
; Thermal imagery
; Thermal infrared imagery
; Thermal infrared imaging
; Infrared imaging
; alpine environment
; energy budget
; ground-based measurement
; heating
; image analysis
; infrared imagery
; spatial distribution
; spatiotemporal analysis
; surface temperature
; temperature gradient
; videography
; Ancash
; Cordillera Blanca
; Cordillera Occidental [Peru]
; Peru
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英文摘要: | Spatially distributed surface temperature is an important, yet difficult to observe, variable for physical glacier melt models. We utilize ground-based thermal infrared imagery to obtain spatially distributed surface temperature data for alpine glaciers. The infrared images are used to investigate thermal microscale processes at the glacier surface, such as the effect of surface cover type and the temperature gradient at the glacier margins on the glacier's temperature dynamics. Infrared images were collected at Cuchillacocha Glacier, Cordillera Blanca, Peru, on 23-25 June 2014. The infrared images were corrected based on ground truth points and local meteorological data. For the control points, the Pearson's correlation coefficient between infrared and station temperatures was 0.95. The ground-based infrared camera has the potential for greatly improving glacier energy budget studies, and our research shows that it is critical to properly correct the thermal images to produce robust, quantifiable data. Key Points Ground based infrared images provide unprecedented glacier temperature data Debris cover increases variability of glacier-surface temperature Heating from glacier's margin is an important energy flux © 2015. American Geophysical Union. All Rights Reserved. |
URL: | https://www.scopus.com/inward/record.uri?eid=2-s2.0-84946606823&doi=10.1002%2f2015GL065321&partnerID=40&md5=98cec5e8aa08b3759f894f55d3f8808b
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Citation statistics: |
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资源类型: | 期刊论文
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标识符: | http://119.78.100.158/handle/2HF3EXSE/8908
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Appears in Collections: | 科学计划与规划 气候变化与战略
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作者单位: | Department of Earth and Planetary Sciences, McGill University, Montreal, QC, Canada
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Recommended Citation: |
Aubry-Wake C.,Baraer M.,McKenzie J.M.,et al. Measuring glacier surface temperatures with ground-based thermal infrared imaging[J]. Geophysical Research Letters,2015-01-01,42(20).
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