How can I fly with the British Airways Unaccompanied Minor Policy?
5_Glacier_IGARSS11_Eineder.ppt
1. GLACIER FLOW AND TOPOGRAPHY MEASUREMENTS WITH TERRASAR-X AND TANDEM-X M. Eineder 1 ) , W. Abdel Jaber 2) , D. Floricioiu 1) , H. Rott 3) , N. Yague-Martinez 1) 1) German Aerospace Center, 2) Technische Universität München, 3) Universität Innsbruck IGARSS 2011
10. Temporal Velocity Profile at Point A (Terminus) Linear fit 2007-2010: -0.166 md -1 a -1 Linear fit 2007/2008: -0.336 md -1 a -1 Summer Winter Summer Winter Summer Winter Significant seasonal variations and decelleration
11. Temporal Velocity Profile at Point C Summer Winter Summer Winter Summer Winter Measurements confirm error margin (residuals stdev. < 2 cm d -1 ) slight seasonal variations, maybe decelleration
18. Difference TanDEM-X (asc) – GLOBE DEM 300 m -300 m 0 m 1. Height loss (?), 2. Velocity and geocoding errors
19.
20.
Editor's Notes
Show position, size History, Larsen A ice shelf break up in Jan 1995 Speedup from 2-3 m/s to 6 m/s in 1995 Why Drygalski Glacier? Have new X-Band TerraSAR-X in 2007 Research, what can be done Fast flowing glacier, accelerated since 1995 What? Show what can be done w.r.t. Velocity tracking 3D Surface mapping Accuracy analysis
Schwimmt in unteren 10 km vermutlich auf
Einsinken bis zu 10 cm / Tag + Tidenhub!!
B <
Massiv außer Balance seit 1995. Starkes Ausdünnen durch Massendivergenz.