191
MODIS-Based Snow Cover Products, Validation, and Hydrologic Applications
Pu et al. (2007)
Tibet Plateau, China
MOD10A2(V004)/2000–2003
Daily SD (115 stations)
84%–91%
Şorman et al. (2007)
Karasu Basin, Turkey
MOD10A1/March 22–25, 2004
Daily SD (24 stations)
100%
Liang et al. (2008a)
Northern Xinjiang, China
MOD10A1 (V004)/November–
March 2002–2005
AMSR-E and daily SD
(20 stations)
93.4% (AMSR-E)
86.7% (stations)
Liang et al. (2008b)
Northern Xinjiang, China
MOD10A1 (V004)/2001–2005
Daily SD (20 stations)
98.5%
Parajka and Blöschl
(2008a)
Austria
MOD10A1 and MYD10A1
(V004)/2003–2005
Daily SD (754 stations)
MYD10A1: 95.5%
MOD10A1: 95.1%
Wang et al. (2008)
Northern Xinjiang, China
MOD10A2 (V004)/2001–2005
Daily SD (20 stations)
93%–97%
Tong et al. (2009b)
Quesnel River Basin, Canada
MOD10A1, MOD10A2
(V005)/2000–2007
Daily SD (4 stations)
MOD10A1: 67.3%–90.1%
MOD10A2: 75.9%–90.1%
Wang et al. (2009)
Northern Xinjiang, China
MOD10A1, MOD10A2,
MYD10A1, MYD10A2 (V004)/
September 2003–August 2004
Daily SD (20 stations)
MOD10A1 and MYD10A1: 98.8%
MOD10A2: 98.1%
MYD10A2: 96.3%
Frei and Lee (2010)
North America
MOD10C1/April–June
(2001–2009)
IMS satellite product and CMC
snow reanalysis
Gao et al. (2010b)
Fairbanks and Upper and
Susitna Valley, Alaska
MOD10A1 and MYD10A1
(V005)/October 2006–September
2007
Daily SD and SWE
(14 stations)
MOD10A1: 94.1%
MYD10A1: 91.6%
Gao et al. (2010a)
Pacific Northwest, U.S.
MOD10A1 and MYD10A1
(V005)/2006–2008
Daily SD (244 SNOTEL
stations)
MOD10A1: 90.4%
MYD10A1: 88.3%
a
OA is defined as the sum of correctly classified (snow–snow, land–land) station-days divided by the total number of station-days (for more details, see, e.g., the work of
Parajka and Blöschl 2008a).
b
Example presented in Figure 9.1.