journal.pone.0195587.pdf (3.612Mb)

Typically the observed ocean heat flux to sea ice is a combination of several factors, including solar heating of the upper layer, salt and heat fluxes from sea ice melt, and the

7 Paper 1: Late summer sea ice segmentation with multi-polarisation SAR features in C- and X-band 43 8 Paper 2: Late summer Arctic Sea Ice Surface Roughness Signatures in C-Band

We have developed a physically based sea-ice albedo parameterization scheme for ECHAM5 GCM following the structure of the sea-ice albedo in a thermo- dynamic sea-ice model [Schramm

In the seawater samples, determination of the temperature, pH, conductivity, salinity, nitrate nitrogen, nitrite nitrogen, ammonia nitrogen, phosphate, alkalinity

Comparisons of winter and summer sea-ice extents at the last glacial maximum (LGM), estimated by the single species proxies with winter and summer sea-ice extents estimated through

Light surfaces such as ice and snow help reduce surface temperatures on earth by reflecting a good deal of solar radiation back to space. It is

Adsorption of nitrate and nitrite by acid treated carbon cloth was tested in a study with the initial concentration of nitrate and nitrite at 115 mg/L, pH was around 7 and

The weak points in all of the reconstruction are the missing magnetic spreading anomalies north of the Greenland Fracture Zone and the lack of any geophysical data along the