• Keine Ergebnisse gefunden

Observation and modeling the iceberg drift in the eastern Weddell Sea iceberg alley

N/A
N/A
Protected

Academic year: 2022

Aktie "Observation and modeling the iceberg drift in the eastern Weddell Sea iceberg alley"

Copied!
1
0
0

Wird geladen.... (Jetzt Volltext ansehen)

Volltext

(1)

Observation and modeling the iceberg drift in the eastern Weddell Sea iceberg alley

Christine Wesche, Thomas Rackow, Wolfgang Dierking

The continental shelf of the eastern Weddell Sea is known as “iceberg alley”.

Icebergs that calve at the coast of East Antarctica drift with the coastal current along the Fimbul Ice Shelf towards the Weddell Sea (Gladstone et al., 2001).

In the beginning of 2006, three large icebergs passed the Ekström Ice Shelf close to the sea ice edge. Using a series of ENVISAT Wide Swath images, they were monitored for nearly one year to investigate the influence of wind, ocean currents, sea ice and the iceberg draft on their drift patterns and to validate corresponding model simulations. The iceberg drift model is driven by the Finite-Elements Sea-ice Ocean Model (FESOM, Timmermann et al., 2009). It was run with a temporal resolution of 6 hours and a spatial resolution of 10 km close to the coast and 30 km further offshore. Besides comparison between iceberg drift observations and computer simulations for improving the model, the observation of icebergs in this region is of great importance for the logistic department at Alfred Wegener Institute because of the supply of the German overwintering station Neumayer III.

The drift of the three icebergs is modeled with different input configurations and parameters. Events with large differences between the modeled and the observed positions are investigated in detail. The goal of this study is to improve the accuracy of the iceberg drift model in the region of the Weddell Sea “drift alley” and thus to be able to forecast iceberg positions as support for marine traffic in this region.

References:

Gladstone, R. M.; Bigg, G. R. & Nicholls, K. W. (2001), Iceberg trajectory modeling and melt water injection in the Southern Ocean, Journal of Geophysical Research, 106(C9), 19903-19915

Timmermann, R.; Danilov, S.; Schröter, J.; Böning, C.; Sidorenko, D. & Rollenhagen, K. (2009), Ocean circulation and sea ice distribution in a finite element global sea ice-ocean model, Ocean Modelling, 27(3-4), 114-129

Referenzen

ÄHNLICHE DOKUMENTE

The results of this lithostratigraphic approach indicate decreasing mean sedimentation rates with increasing water depth on a profile across the continental slope in the

Comparison between iceberg path (#9367) with 24-h sampling interval and sea-ice buoy # 8060 with 3-h sampling interval for the circled area in top panel (bottom). The blue

Optimized values for the drag coefficients and for the ice strength parameter are determined by applying the error function to various sensitivity studies with

Thomas J A, Stirling I (1983) Geographic variation in the underwater vocalizations of Weddell seals (Leptonychotes weddellii) from Palmer Peninsula and McMurdo Sound,

This report summarises visual shipboard ice observations carried out during leg ARKTIS 17/2 (ARK 17/2) of RV POLARSTERN in August and September 2001, operating along the Gakkel

It is shown that the temperature distribution and related thermal properties of snow-covered sea ice can be represented by a one-dimensional thermody- namic sea ice model, on

Numbers of identified squid beaks ffom stomach contents of adult emperor penguins and estimated wet mass represented by beaks.. Beaks are separated into degradation classes A, B and

Consequent- ly Hopkins (1985a) did not find neritic species, like Euphausia crystallorophias, and meroplanktonic larvae, which were abundant in the coastal Weddell