Multitemporal snow cover mapping in mountainous terrain for Landsat climate data record development

被引:59
作者
Crawford, Christopher J. [1 ]
Manson, Steven M. [1 ]
Bauer, Marvin E. [2 ]
Hall, Dorothy K. [3 ]
机构
[1] Univ Minnesota Twin Cities, Dept Geog, Minneapolis, MN 55455 USA
[2] Univ Minnesota Twin Cities, Dept Forest Resources, St Paul, MN 55108 USA
[3] NASA, Cryospher Sci Lab, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
关键词
Landsat; Multitemporal; Snow cover; Climate data record; Mountains; CLOUD-COVER; TM DATA; REFLECTANCE; VARIABILITY; ACCURACY; ETM+; PRECIPITATION; TEMPERATURE; RESOLUTION; TRENDS;
D O I
10.1016/j.rse.2013.04.004
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
A multitemporal method to map snow cover in mountainous terrain is proposed to guide Landsat climate data record (CDR) development. The Landsat image archive including MSS, TM, and ETM + imagery was used to construct a prototype Landsat snow cover CDR for the interior northwestern United States. Landsat snow cover CDRs are designed to capture snow-covered area (SCA) variability at discrete bi-monthly intervals that correspond to ground-based snow telemetry (SNOTEL) snow-water-equivalent (SWE) measurements. The June 1 bi-monthly interval was selected for initial CDR development, and was based on peak snowmelt timing for this mountainous region. Fifty-four Landsat images from 1975 to 2011 were preprocessed that included image registration, top-of-the-atmosphere (TOA) reflectance conversion, cloud and shadow masking, and topographic normalization. Snow covered pixels were retrieved using the normalized difference snow index (NDSI) and unsupervised classification, and pixels having greater (less) than 50% snow cover were classified presence (absence). A normalized SCA equation was derived to independently estimate SCA given missing image coverage and cloud-shadow contamination. Relative frequency maps of missing pixels were assembled to assess whether systematic biases were embedded within this Landsat CDR. Our results suggest that it is possible to confidently estimate historical bi-monthly SCA from partially cloudy Landsat images. This multitemporal method is intended to guide Landsat CDR development for freshwater-scarce regions of the western US to monitor climate-driven changes in mountain snowpack extent. (C) 2013 Elsevier Inc. All rights reserved.
引用
收藏
页码:224 / 233
页数:10
相关论文
共 72 条
[1]   Discriminating clear sky from clouds with MODIS [J].
Ackerman, SA ;
Strabala, KI ;
Menzel, WP ;
Frey, RA ;
Moeller, CC ;
Gumley, LE .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1998, 103 (D24) :32141-32157
[2]  
[Anonymous], 2013, ADV WATER RESOUR, DOI [DOI 10.1016/J.ADVWATRES.2012.03.002, DOI 10.1016/j.advwatres.2012.03.002]
[3]   Potential impacts of a warming climate on water availability in snow-dominated regions [J].
Barnett, TP ;
Adam, JC ;
Lettenmaier, DP .
NATURE, 2005, 438 (7066) :303-309
[4]  
Barry R.G., 2002, Polar Geography, V26, P235, DOI DOI 10.1080/789610195
[5]   Northern Hemisphere spring snow cover variability and change over 1922-2010 including an assessment of uncertainty [J].
Brown, R. D. ;
Robinson, D. A. .
CRYOSPHERE, 2011, 5 (01) :219-229
[6]  
Cayan DR, 2001, B AM METEOROL SOC, V82, P399, DOI 10.1175/1520-0477(2001)082<0399:CITOOS>2.3.CO
[7]  
2
[8]  
Cayan DR, 1996, J CLIMATE, V9, P928, DOI 10.1175/1520-0442(1996)009<0928:ICVASI>2.0.CO
[9]  
2
[10]   Revised Landsat-5 TM radiometric calibration procedures and postcalibration dynamic ranges [J].
Chander, G ;
Markham, B .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 2003, 41 (11) :2674-2677