MISR-based passive optical bathymetry from orbit with few-cm level of accuracy on the Salar de Uyuni, Bolivia

被引:17
作者
Bills, Bruce G. [1 ]
Borsa, Adrian A.
Comstock, Robert L.
机构
[1] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
[2] Scripps Inst Oceanog, La Jolla, CA USA
关键词
MISR; topography; bathymetry; passive optical; Salar de Uyuni;
D O I
10.1016/j.rse.2006.11.006
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
We demonstrate that, under ideal circumstances, passive optical measurements can yield surface water depth estimates with an accuracy of a few centimeters. Our target area is the Salar de Uyuni, in Bolivia. It is a large, active salt flat or playa, which is maintained as an almost perfectly le vel and highly reflective surface by annual flooding, to a mean depth of 30-50 cm. We use MISR data to estimate spatial and temporal variations in water depth during the waning portion of the 2001 flooding cycle. We use a single ICESat laser altimetry profile to calibrate our water depth model.-Though the salt surface is probably the smoothest surface of its size on Earth, with less that 30 cm RMS height variations over an area of nearly 10(4) km(2), it is not completely featureless. Topography there includes a peripheral depression, or moat, around the edge of the salt, and several sets of prominent parallel ridges, with 5 km wavelength and 30 cm amplitude. The process by which these features form is still not well characterized. (c) 2006 Elsevier Inc. All rights reserved.
引用
收藏
页码:240 / 255
页数:16
相关论文
共 114 条
[91]   QUATERNARY GEOCHEMICAL EVOLUTION OF THE SALARS OF UYUNI AND COIPASA, CENTRAL ALTIPLANO, BOLIVIA [J].
RISACHER, F ;
FRITZ, B .
CHEMICAL GEOLOGY, 1991, 90 (3-4) :211-231
[92]   Bromine geochemistry of salar de Uyuni and deeper salt crusts, Central Altiplano, Bolivia [J].
Risacher, F ;
Fritz, B .
CHEMICAL GEOLOGY, 2000, 167 (3-4) :373-392
[93]  
Roche M.A, 1992, LAKE TITICACA SYNTHE, P63, DOI DOI 10.1007/978-94-011-2406-5_4
[94]   The cross-sectional shape of tidal sandbanks: Modeling and observations [J].
Roos, PC ;
Hulscher, SJMH ;
Knaapen, MAF ;
Van Damme, RMJ .
JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE, 2004, 109 (F2)
[95]  
Rosen Michael R, 1994, PALEOCLIMATE BASIN E, V289, P1
[96]   Extensive carbonate algal bioherms in upper Pleistocene saline lakes of the central Altiplano of Bolivia [J].
Rouchy, JM ;
Servant, M ;
Fournier, M ;
Causse, C .
SEDIMENTOLOGY, 1996, 43 (06) :973-993
[97]   Hydrologic-energy balance constraints on the Holocene lake-level history of lake Titicaca, South America [J].
Rowe, HD ;
Dunbar, RB .
CLIMATE DYNAMICS, 2004, 23 (3-4) :439-454
[98]   Coastal bathymetry from hyperspectral observations of water radiance [J].
Sandidge, JC ;
Holyer, RJ .
REMOTE SENSING OF ENVIRONMENT, 1998, 65 (03) :341-352
[99]   Error characteristics estimated from CHAMP, GRACE and GOCE derived geoids and from satellite altimetry derived mean dynamic topography [J].
Schrama, EJO .
SPACE SCIENCE REVIEWS, 2003, 108 (1-2) :179-193
[100]  
SERVANT M, 1978, CAH OSTROM, V10, P2