journal.pone.0195587.pdf (3.612Mb)

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

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

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

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

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