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Glacier elevation and mass changes over the central Karakoram region estimated from TanDEM-X and SRTM/X-SAR digital elevation models

Published online by Cambridge University Press:  03 March 2016

Melanie Rankl  and
Matthias Braun
Melanie Rankl*
Affiliation:
Institute of Geography, University of Erlangen–Nuremberg, Erlangen, Germany
Matthias Braun
Affiliation:
Institute of Geography, University of Erlangen–Nuremberg, Erlangen, Germany
*
Correspondence: Melanie Rankl <[email protected]>
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Abstract

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Snow cover and glaciers in the Karakoram region are important freshwater resources for many down-river communities as they provide water for irrigation and hydropower. A better understanding of current glacier changes is hence an important informational baseline. We present glacier elevation changes in the central Karakoram region using TanDEM-X and SRTM/X-SAR DEM differences between 2000 and 2012. We calculated elevation differences for glaciers with advancing and stable termini or surge-type glaciers separately using an inventory from a previous study. Glaciers with stable and advancing termini since the 1970s showed nearly balanced elevation changes of -0.09 ±0.12 m a-1 on average or mass budgets of -0.01 ±0.02Gt a-1 (using a density of 850 kg m-3). Our findings are in accordance with previous studies indicating stable or only slightly negative glacier mass balances during recent years in the Karakoram. The high-resolution elevation changes revealed distinct patterns of mass relocation at glacier surfaces during active surge cycles. The formation of kinematic waves at quiescent surge-type glaciers could be observed and points towards future active surge behaviour. Our study reveals the potential of the TanDEM-X mission to estimate geodetic glacier mass balances, but also points to still existing uncertainties induced by the geodetic method.

Keywords

glacier mass balanceglacier surgesmountain glaciersremote sensing
Type
Paper
Information
Annals of Glaciology , Volume 57 , Issue 71 , March 2016 , pp. 273 - 281
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited.
Copyright
Copyright © The Author(s) 2016

References

Archer, D and Fowler, H (2004) Spatial and temporal variations in precipitation in the Upper Indus Basin: global teleconnections and hydrological implications. Hydrol. Earth Syst. Sci. 8(1), 47–61 (doi: 10.5194/hess-8-47-2004)CrossRefGoogle Scholar
Barrand, NE and Murray, T (2006) Multivariate controls on the incidence of glacier surging in the Karakoram Himalaya. Arct. Antarct. Alp. Res., 38(4), 489–498 (doi: 10.1657/1523-0430 (2006)38[489:MCOTIO]2.0.CO;2)CrossRefGoogle Scholar
Berthier, E, Arnaud, Y, Vincent, C and Rémy, F (2006) Biases of SRTM in high-mountain areas: implications for the monitoring of glacier volume changes. Geophys. Res. Lett., 33(8) (doi: 10.1029/2006GL025862)Google Scholar
Berthier, E, Arnaud, Y, Kumar, R, Ahmad, S, Wagnon, P and Chevallier, P (2007) Remote sensing estimates of glacier mass balances in the Himachal Pradesh (Western Himalaya, India). Remote Sens. Environ., 108(3), 327–338 (doi: 10.1016/j.rse.2006.11.017)CrossRefGoogle Scholar
Bolch, T and 11 others (2012) The state and fate of Himalayan glaciers. Science 336(6079), 310–314 (doi: 10.1126/science. 1215828)Google Scholar
Clarke, GK, Collins, S and Thompson, D (1984) Flow, thermal structure, and subglacial conditions of a surge-type glacier. Can. J. Earth Sci., 21(2), 232–240 (doi: 10.1139/e84-024)Google Scholar
Copland, L and 7 others (2011) Expanded and recently increased glacier surging in the Karakoram. Arct. Antarct. Alp. Res. 43(4), 503–516 (doi: 10.1657/1938-4246-43.4.503)Google Scholar
Fritz, T, Rossi, C, Yague-Martinez, N, Rodriguez-Gonzalez, F, Lachaise, M and Breit, H (2011) Interferometric processing of TanDEM-X data. In IGARSS 2011, International Geoscience and Remote Sensing Symposium, 24–29 July 2011, Vancouver, B.C., Canada. Proceedings. Institute of Electrical and Electronics Engineers, Piscataway, NJ, 2428–2431 (doi: 10.1109/IGARSS.2011.6049701)Google Scholar
Gamma Remote Sensing (2007) GAMMA Differential Interferometry and Geocoding Software (DIFF/GEO). Gamma Remote Sensing, GumligenGoogle Scholar
Gardelle, J, Berthier, E and Arnaud, Y (2012) Impact of resolution and radar penetration on glacier elevation changes computed from DEM differencing. J. Glaciol., 58(208), 419–422 (doi: 10.3189/2012JoG11J175)Google Scholar
Gardelle, J, Berthier, E, Arnaud, Y and Kääb, A (2013) Region-wide glacier mass balances over the Pamir–Karakoram–Himalaya during 1999–2011. Cryosphere, 7(4), 1263–1286 (doi: 10.5194/tc-7-1263-2013)Google Scholar
Gardner, AS and 9 others (2013) A reconciled estimate of glacier contributions to sea level rise: 2003 to 2009. Science, 340(6134), 852–857 (doi: 10.1126/science.1234532)CrossRefGoogle ScholarPubMed
Goldstein, RM and Werner, CL (1998) Radar interferogram filtering for geophysical applications. Geophys. Res. Lett., 25(21), 4035–4038 (doi: 10.1029/1998GL900033)CrossRefGoogle Scholar
Groh, A and 11 others (2014) Mass, volume and velocity of the Antarctic ice sheet: present-day changes and error effects. Surv. Geophys., 35(6), 1481–1505 (doi: 10.1007/s10712-014-9286-y)Google Scholar
Hewitt, K (1969) Glacier surges in the Karakoram Himalaya (central Asia). Can. J. Earth Sci. 6(4), 1009–1018 (doi: 10.1139/e69-106)CrossRefGoogle Scholar
Hewitt, K (1998) Recent glacier surges in the Karakoram Himalaya, South Central Asia. Eos, 79(8), 104–105 Google Scholar
Hewitt, K (2007) Tributary glacier surges: an exceptional concentration at Panmah Glacier, Karakoram Himalaya. J. Glaciol. 53(181), 181–188 (doi: 10.3189/172756507782202829)Google Scholar
Hewitt, K (2014) Glaciers of the Karakoram Himalaya: glacial environments, processes, hazards and resources. Springer, Berlin Google Scholar
Hoffmann, J and Walter, D (2006) How complementary are SRTM-X and-C band digital elevation models? Photogramm. Eng. Remote Sens., 72(3), 261–268 (doi: 10.14358/PERS.72.3.261)CrossRefGoogle Scholar
Huss, M (2013) Density assumptions for converting geodetic glacier volume change to mass change. Cryosphere 7(3), 877–887 (doi: 10.5194/tc-7-877-2013)Google Scholar
Immerzeel, WW, Van Beek, LP and Bierkens, MF (2010) Climate change will affect the Asian water towers. Science, 328(5984), 1382–1385 (doi: 10.1126/science.1183188)Google Scholar
Kääb, A, Berthier, E, Nuth, C, Gardelle, J and Arnaud, Y (2012) Contrasting patterns of early twenty-first-century glacier mass change in the Himalayas. Nature 488(7412), 495–498 (doi: 10.1038/nature11324)CrossRefGoogle ScholarPubMed
Kääb, A, Treichler, D, Nuth, C and Berthier, E (2015) Brief Communication: Contending estimates of 2003–2008 glacier mass balance over the Pamir–Karakoram–Himalaya. Cryosphere, 9(2), 557–564 (doi: 10.5194/tc-9-557-2015)Google Scholar
Kapnick, SB, Delworth, TL, Ashfaq, M, Malyshev, S and Milly, PCD (2014) Snowfall less sensitive to warming in Karakoram than in Himalayas due to a unique seasonal cycle. Nature Geosci., 7(11), 834–840 (doi: 10.1038/ngeo2269)CrossRefGoogle Scholar
Kaser, G, Großhauser, M and Marzeion, B (2010) Contribution potential of glaciers to water availability in different climate regimes. Proc. Natl Acad. Sci., 107(47), 20 223–20 227 (doi: 10.1073/pnas.1008162107)Google Scholar
Kienholz, C, Rich, JL, Arendt, AA and Hock, R (2014) A new method for deriving glacier centerlines applied to glaciers in Alaska and northwest Canada. Cryosphere 8(2), 503–519 (doi: 10.5194/tc- 8-503-2014)CrossRefGoogle Scholar
Krieger, G and 6 others (2007) TanDEM-X: a satellite formation for high-resolution SAR interferometry. IEEE Trans. Geosci. Remote Sens., 45(11), 3317–3341 (doi: 10.1109/TGRS.2007.900693)Google Scholar
Ludwig, R and Schneider, P (2006) Validation of digital elevation models from SRTM X-SAR for applications in hydrologic modeling. ISPRS J. Photogramm. Remote Sens., 60(5), 339–358 (doi: 10.1016/j.isprsjprs.2006.05.003)Google Scholar
Marzeion, B, Jarosch, AH and Hofer, M (2012) Past and future sealevel change from the surface mass balance of glaciers. Cryosphere 6(6), 1295–1322 (doi: 10.5194/tc-6-1295-2012)Google Scholar
Mätzler, C and Schanda, E (1984) Snow mapping with active microwave sensors. Remote Sens., 5(2), 409–422 (doi: 10.1080/01431168408948816)CrossRefGoogle Scholar
Mayer, C, Fowler, A, Lambrecht, A and Scharrer, K (2011) A surge of North Gasherbrum Glacier, Karakoram, China. J. Glaciol., 57(205), 904–916 (doi: 10.3189/002214311798043834)CrossRefGoogle Scholar
Meier, MF and Post, A (1969) What are glacier surges? Can. J. Earth Sci., 6(4), 807–817 (doi: 10.1139/e69-081)Google Scholar
Moholdt, G, Nuth, C, Hagen, JO and Kohler, J (2010) Recent elevation changes of Svalbard glaciers derived from ICESat laser altimetry. Remote Sens. Environ., 114(11), 2756–2767 (doi: 10.1016/j.rse.2010.06.008)Google Scholar
Mölg, T, Maussion, F and Scherer, D (2014) Mid-latitude westerlies as a driver of glacier variability in monsoonal High Asia. Nature Climate Change, 4(1), 68–73 (doi: 10.1038/nclimate2055)CrossRefGoogle Scholar
Neckel, N, Braun, A, Kropáček, J and Hochschild, V (2013) Recent mass balance of the Purogangri Ice Cap, central Tibetan Plateau, by means of differential X-band SAR interferometry. Cryosphere, 7(5), 1623–1633 (doi: 10.5194/tc-7-1623-2013)Google Scholar
Neckel, N, Kropáček, J, Bolch, T and Hochschild, V (2014) Glacier mass changes on the Tibetan Plateau 2003–2009 derived from ICESat laser altimetry measurements. Environ. Res. Lett., 9(1), 014009 (doi: 10.1088/1748-9326/9/1/014009)Google Scholar
Quincey, DJ, Braun, M, Glasser, NF, Bishop, MP, Hewitt, K and Luckman, A (2011) Karakoram glacier surge dynamics. Geophys Res. Lett., 38, L18504 (doi: 10.1029/2011GL049004)Google Scholar
Radić, V and Hock, R (2011) Regionally differentiated contribution of mountain glaciers and ice caps to future sea-level rise. Nature Geosci., 4(2), 91–94 (doi: 10.1038/ngeo1052)Google Scholar
Rankl, M, Kienholz, C and Braun, M (2014) Glacier changes in the Karakoram region mapped by multimission satellite imagery. Cryosphere 8(3), 977–989 (doi: 10.5194/tc-8-977-2014)Google Scholar
Rignot, E, Echelmeyer, K and Krabill, W (2001) Penetration depth of interferometric synthetic-aperture radar signals in snow and ice. Geophys. Res. Lett., 28(18), 3501–3504 (doi: 10.1029/2000GL012484)Google Scholar
Scherler, D, Bookhagen, B and Strecker, M. (2011) Spatially variable response of Himalayan glaciers to climate change affected by debris cover. Nature Geosci., 4(3), 156–159 (doi: 10.1038/ngeo1068)Google Scholar
Schiefer, E, Menounos, B and Wheate, R (2007) Recent volume loss of British Columbian glaciers, Canada. Geophys. Res. Lett., 34(16), L16503 (doi: 10.1029/2007GL030780)Google Scholar
Seehaus, T, Marinsek, S, Helm, V, Skvarca, P and Braun, M (2015) Changes in ice dynamics, elevation and mass discharge of Dinsmoor–Bombardier–Edgeworth glacier system, Antarctic Peninsula. Earth Planet. Sci. Lett., 427, 125–135 (doi: 10.1016/j.epsl.2015.06.047)Google Scholar
Shuman, CA, Berthier, E and Scambos, TA (2011) 2001–2009 elevation and mass losses in the Larsen A and B embayments, Antarctic Peninsula. J. Glaciol., 57(204), 737–754 (doi: 10.3189/002214311797409811)Google Scholar
Ulaby, FT, Moore, RK and Fung, AK (1986) Microwave remote sensing, active and passive. Vol. III: From theory to applications. Artech House, Norwood, MA Google Scholar
Werner, C, Wegmüller, U, Strozzi, T and Wiesmann, A (2000) Gamma SAR and interferometric processing software. Proceedings of the ERS–ENVISAT Symposium, Gothenburg, Sweden, 16–20 October 2000. European Space Agency, Noordwijk Google Scholar
Yao T and 9 others (2012) Different glacier status with atmospheric circulations in Tibetan Plateau and surroundings. Nature Climate Change, 2(9), 663–667 (doi: 10.1038/nclimate1580)Google Scholar