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Faculty of Environmental Sciences, Institute of Cartography Zhadang Glacier Orthorectification of terrestrial time-lapse camera images for snow line mapping Benjamin Schrter , Tino Pieczonka, Jan Kropek, Manfred Buchroithner Technische


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Faculty of Environmental Sciences, Institute of Cartography

Zhadang Glacier Orthorectification of terrestrial time-lapse camera images for snow line mapping

Benjamin Schröter, Tino Pieczonka, Jan Kropáček, Manfred Buchroithner Technische Universität Dresden, Institute of Cartography

9th ICA Workshop on Mountain Cartography, Banff (Canada), 22-26 April 2014

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Faculty of Environmental Sciences, Institute of Cartography

Outline

  • 1. Motivation
  • 2. Investigation area – Zhadang Glacier
  • 3. Terrestrial time-lapse camera system
  • 4. Orthorectification – method and workflow
  • 5. Results
  • 6. Conclusion/Outlook
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Faculty of Environmental Sciences, Institute of Cartography

Motivation

  • 1. Glaciers are key indicators for the ongoing climate change
  • 2. The covering snowpack considerably affects the glacier-ice surface temperature

and thus the meltdown of the glaciers

  • 3. The detailed investigation as well as the accurate delineation of the actual snow

line – here defined as the fluctuating lower altitudinal boundary of the snow- covered area – are of high importance

  • 4. Evaluation and validation of a glacier mass balance model developed at RWTH

Aachen

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Faculty of Environmental Sciences, Institute of Cartography

Tibet

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Framework within research projects: TiP and WET

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Faculty of Environmental Sciences, Institute of Cartography

Nam Co Lhasa Nyainqêntanglha Range

Zhadang Glacier

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Faculty of Environmental Sciences, Institute of Cartography

Zhadang Glacier (5,515 – 6,090 m a.s.l., 2 km2)

Photo: T. Pieczonka (2009)

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Titel der Präsentation Folie Nr. 8 von XYZ

Terrestrial camera system, Zhadang Glacier

Photo: T. Pieczonka (2009)

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Faculty of Environmental Sciences, Institute of Cartography

Map: E. Huintjes (2013)

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Terrestrial camera system, Zhadang Glacier 2010/2011

picture series from 2010 picture series from 2011

2 cameras, each 6 pictures/day = 6,225 images between May 2010 and September 2012

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Faculty of Environmental Sciences, Institute of Cartography

Terrestrial camera system, Zhadang Glacier Cam1/Cam2

picture series 2011 from Cam 1 picture series 2011 from Cam 2

2 cameras, each 6 pictures/day = 6,225 images between May 2010 and September 2012

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Faculty of Environmental Sciences, Institute of Cartography

Problem: movement/shift of both cameras due to melting/refreezing or possibly earthquake

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Faculty of Environmental Sciences, Institute of Cartography

Orthorectification of the camera images with software RSG (Remote Sensing Software Graz)

  • 1. Manual orthorectification (1 image/week/camera), detection of the image

coordinates of the GCPs (change because of camera movement)

  • 2. Renaming of all images (scheme cam1_20110716_14)
  • 3. Interpolation of image coordinates of the GCPs and generation of a .cl (column-

line) file for every image (same file name like corresponding image)

  • 4. Selection of „good“ GCPs with lowest residuals (cam 1: 6 GCPs, cam 2: 5 GCPs)
  • 5. Batch-processing (reference is SRTM – resampled to 1 m, image and interpolated

image coordinates of the GCPs are connected by the file names)

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Faculty of Environmental Sciences, Institute of Cartography

7 GCPs that can be identified in every picture (repeatedly measured in the field)

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Faculty of Environmental Sciences, Institute of Cartography

Orthorectified area of Zhadang Glacier (Image distortion due to very gentle rise of the

upper part of the glacier)

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Faculty of Environmental Sciences, Institute of Cartography

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Faculty of Environmental Sciences, Institute of Cartography

Example of workflow image to ortho-image with snowline

Camera 1: view towards south

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Faculty of Environmental Sciences, Institute of Cartography

Nadir view, northened

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Faculty of Environmental Sciences, Institute of Cartography

Snowline on nadir view

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Faculty of Environmental Sciences, Institute of Cartography

  • A remarkable result is the proof of the existence of

ablation due to heavy snow drift and sublimation

  • n the glacier during the winter months (DJFM)
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Faculty of Environmental Sciences, Institute of Cartography

Image from February 6 2012 at 22:00

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Faculty of Environmental Sciences, Institute of Cartography

Conclusions/Outlook

  • 1. Considerable variability and fluctuation of the snow lines
  • 2. Proof of snow drift and sublimation
  • 3. Automatization of the process
  • 4. GLOF monitoring in Halji, Nepal
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Pléiades DEM (2013), 1 m resolution Pléiades DEM (2013) to SRTM-3 (2000)

  • N. Holzer (2013)

Halji-Glacier

  • N. Holzer (2013)
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Faculty of Environmental Sciences, Institute of Cartography

SFM

DEM based on fusion of SFM and DGPS measurements Morphometry of the lake basin First GLOF modeling results

  • B. Tyrna (2014)
  • N. Neckel (2014)
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Faculty of Environmental Sciences, Institute of Cartography

Automatic Weather Station Terrestrial Camera

Photos: B. Schröter (2014)

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Faculty of Environmental Sciences, Institute of Cartography

TU Dresden >> Faculty of Forest, Geo and Hydro Sciences >> Institute of Cartography

Further questions: benjamin.schroeter@tu-dresden.de

Thank you very much for your attention!

Nicolai Holzer: TU Dresden

Thanks to:

Eva Huintjes: RWTH Aachen Niklas Neckel: Eberhard Karls Universität Tübingen