Hermann Schomberg als Sir John Falstaff, Rollenbild, Brustbild, in: William Shakespeare (Gobert George): König Heinrich IV., Frankfurt a. M.: Römerbergfestspiele, 1937

Signatur des Originals: S 36/F12150

Hermann Schomberg als Sir John Falstaff, Rollenbild, in: William Shakespeare (Robert George): König Heinrich IV., Frankfurt a. M.: Römerbergfestspiele, 1937

Signatur des Originals: S 36/F12152

Elizabeth Bannister als Patty, George Mattocks als Lord Aimworth, Szenenfoto, Doppelbildnis, in: Samuel Arnold: The Maid of the Mill, II. Akt, 3. Szene : Patty: "Cease, oh cease, to overwhelm me"

Signatur des Originals: S 36/G00065

George Frederick Handel : Handel's Monument in Westminster Abbey

Signatur des Originals: S 36/G01068

George Frederick Handel

Signatur des Originals: S 36/G01074

George Frederic Handel

Signatur des Originals: S 36/G01075

George Frederick Handel

Signatur des Originals: S 36/G01076

George Fred. Handel

Signatur des Originals: S 36/G01079

George Thomas Smart, Brustbild

Signatur des Originals: S 36/G02260

George Grove, Brustbild

Signatur des Originals: S 36/G03102

George Jackson Lambert, Brustbild

Signatur des Originals: S 36/G03268

George Jackson Lambert, Brustbild

Signatur des Originals: S 36/G03269

George Alexander Osborne, Brustbild

Signatur des Originals: S 36/G04277

George Perry, Brustbild

Signatur des Originals: S 36/G04301

Snow and ice surfaces on King George Island (Antarctic Peninsula) with high-resolution TerraSAR-X time series, with links to shapfiles and GeoTIFFs

Changes of glaciers and snow cover in polar regions affect a wide range of physical and ecosystem processes on land and in the adjacent marine environment. In this study, we investigate the potential of 11-day repeat high-resolution satellite image time series from the TerraSAR-X mission to derive glaciological and hydrological parameters on King George Island, Antarctica during the period Oct/25/2010 to Apr/19/2011. The spatial pattern and temporal evolution of snow cover extent on ice-free areas can be monitored using multi-temporal coherence images. SAR coherence is used to map glacier extent of land terminating glaciers with an average accuracy of 25 m. Multi-temporal SAR color composites identify the position of the late summer snow line at about 220 m above sea level. Glacier surface velocities are obtained from intensity feature-tracking. Surface velocities near the calving front of Fourcade Glacier were up to 1.8 ± 0.01 m/d. Using an intercept theorem based on fundamental geometric principles together with differential GPS field measurements, the ice discharge of Fourcade Glacier was estimated to 20700 ± 5500 m**3/d (corresponding to ~19 ± 5 kt/d). The rapidly changing surface conditions on King George Island and the lack of high-resolution digital elevation models for the region remain restrictions for the applicability of SAR data and the precision of derived products.