Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Zhang, Guoqing; Xie, Hongjie; Kang, Shichang; Yi, Donghui; Ackley, Stephen F (2011): (Table 1) Lake elevation change derived from 4 or more years of measurements [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.842774, Supplement to: Zhang, G et al. (2011): Monitoring lake level changes on the Tibetan Plateau using ICESat altimetry data (2003-2009). Remote Sensing of Environment, 115(7), 1733-1742, https://doi.org/10.1016/j.rse.2011.03.005

Always quote citation above when using data! You can download the citation in several formats below.

RIS CitationBibTeX CitationShow MapGoogle Earth

Abstract:
In this study, ICESat altimetry data are used to provide precise lake elevations of the Tibetan Plateau (TP) during the period of 2003-2009. Among the 261 lakes examined ICESat data are available on 111 lakes: 74 lakes with ICESat footprints for 4-7 years and 37 lakes with footprints for 1 -3 years. This is the first time that precise lake elevation data are provided for the 111 lakes. Those ICESat elevation data can be used as baselines for future changes in lake levels as well as for changes during the 2003-2009 period. It is found that in the 74 lakes (56 salt lakes) examined, 62 (i.e. 84%) of all lakes and 50 (i.e. 89%) of the salt lakes show tendency of lake level increase. The mean lake water level increase rate is 0.23 m/year for the 56 salt lakes and 0.27 m/year for the 50 salt lakes of water level increase. The largest lake level increase rate (0.80 m/year) found in this study is the lake Cedo Caka. The 74 lakes are grouped into four subareas based on geographical locations and change tendencies in lake levels. Three of the four subareas show increased lake levels. The mean lake level change rates for subareas I, II, III, IV, and the entire TP are 0.12, 0.26, 0.19, -0.11, and 0.2 m/year, respectively. These recent increases in lake level, particularly for a high percentage of salt lakes, supports accelerated glacier melting due to global warming as the most likely cause.
Coverage:
Median Latitude: 33.127986 * Median Longitude: 88.446092 * South-bound Latitude: 28.567210 * West-bound Longitude: 80.899580 * North-bound Latitude: 38.302450 * East-bound Longitude: 100.170000
Minimum ELEVATION: 3193.35 m a.s.l. * Maximum ELEVATION: 5115.74 m a.s.l.
Event(s):
Argog_Co * Latitude: 30.987430 * Longitude: 82.235040 * Location: Tibetan Plateau * Method/Device: Multiple investigations (MULT)
Baqan_Co * Latitude: 31.923620 * Longitude: 82.783590 * Location: Tibetan Plateau * Method/Device: Multiple investigations (MULT)
Cedo_Caka * Latitude: 33.181400 * Longitude: 89.031070 * Location: Tibetan Plateau * Method/Device: Multiple investigations (MULT)
Comment:
Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEvent
2Latitude of eventLatitude
3Longitude of eventLongitude
4LakeLakeZhang, Guoqing
5NumberNoZhang, GuoqingICESat satellite dataof ICESat tracks within no. of years
6Number of yearsYearsaZhang, GuoqingICESat satellite data
7NumberNoZhang, GuoqingICESat satellite dataof footprints per track, mean
8ELEVATIONElevationm a.s.l.Geocode
9Date/time startDate/time startZhang, GuoqingICESat satellite data
10Elevation 2Elev2m a.s.l.Zhang, GuoqingICESat satellite dataat end
11Date/time endDate/time endZhang, GuoqingICESat satellite data
12Standard deviationStd dev±Zhang, GuoqingICESat satellite datamean
13Water level changeWL changem/aZhang, GuoqingICESat satellite data
14Lake typeLake typeZhang, GuoqingF = fresh, S = salt
15SectorSectorZhang, Guoqing
Size:
814 data points

Download Data

Download dataset as tab-delimited text — use the following character encoding:

View dataset as HTML