We present a process study on the dynamics and variability of the Terra Nova Bay polynya in the western sector of the Ross Sea. The air-sea heat exchange is known to be particularly large in polynyas during the winter, when differences between air and sea temperatures are large. We apply a 1-D model (Pease, 1987; Van Woert, 1999a, 1999b), which is modified in the latent heat parameterisation in order to account for time-dependent relative humidity and cloud coverage. Furthermore, the Ice Collection Depth is correlated linearly with a variable wind speed. The model is forced with two different meteorological data sets: the operational analysis of the European Center for Medium Range Weather Forecasts atmospheric data set and the meteorologic...
The variation of Ross Ice Shelf Polynya (RISP) ice production is a synergistic result of several fac...
The density and salinity of High Salinity Shelf Water, a key component of Antarctic Bottom Water ema...
An event of polynya at Terra Nova Bay (TNB),occurring from 15 July to 17 July 2006, is simulated by ...
We present a process study on the dynamics and variability of the Terra Nova Bay polynya in the west...
The Terra Nova Bay (TNB) and Ross Ice Shelf (RIS) polynyas are simulated using a coupled atmosphere–...
A rare long time series of hydrographic profiles and moored current meter data, collected from 1995 ...
Antarctic sea ice is constantly exported from the shore by strong near surface winds that open leads...
The Ross Sea is characterized by the presence of persistent ice-free areas during the austral winter...
The energy exchange between the ocean and the atmosphere in the Antarctic marginal sea ice zone is i...
Polynyas play an important role in the meteorology and oceanography of the polar regions and in the ...
Coastal polynyas around Antarctica are the place of intense air–sea exchanges which eventually lead ...
Coastal polynyas are areas of partially or totally ice free water which form in coastal regions duri...
Antarctic sea ice formation is strongly influenced by polynyas occurring in austral winter. The sea ...
We investigate the impacts of strong wind events on the sea ice concentration within the Ross Sea po...
The variation of Ross Ice Shelf Polynya (RISP) ice production is a synergistic result of several fac...
The density and salinity of High Salinity Shelf Water, a key component of Antarctic Bottom Water ema...
An event of polynya at Terra Nova Bay (TNB),occurring from 15 July to 17 July 2006, is simulated by ...
We present a process study on the dynamics and variability of the Terra Nova Bay polynya in the west...
The Terra Nova Bay (TNB) and Ross Ice Shelf (RIS) polynyas are simulated using a coupled atmosphere–...
A rare long time series of hydrographic profiles and moored current meter data, collected from 1995 ...
Antarctic sea ice is constantly exported from the shore by strong near surface winds that open leads...
The Ross Sea is characterized by the presence of persistent ice-free areas during the austral winter...
The energy exchange between the ocean and the atmosphere in the Antarctic marginal sea ice zone is i...
Polynyas play an important role in the meteorology and oceanography of the polar regions and in the ...
Coastal polynyas around Antarctica are the place of intense air–sea exchanges which eventually lead ...
Coastal polynyas are areas of partially or totally ice free water which form in coastal regions duri...
Antarctic sea ice formation is strongly influenced by polynyas occurring in austral winter. The sea ...
We investigate the impacts of strong wind events on the sea ice concentration within the Ross Sea po...
The variation of Ross Ice Shelf Polynya (RISP) ice production is a synergistic result of several fac...
The density and salinity of High Salinity Shelf Water, a key component of Antarctic Bottom Water ema...
An event of polynya at Terra Nova Bay (TNB),occurring from 15 July to 17 July 2006, is simulated by ...