Satellite-Derived Thermal Infrared Data"

For example, the warm shear (WSR) and the cold dense regime (CDR) do not differ much in the MTI flowing signature, both are homogeneous and can have similar velocities, but the

Combining our new results with existing data in the region, we produce a grid of the sub-ice shelf bathymetry and water column thickness, revealing new features that help enhance

By performing moisture and MSE budgets on reanalysis and climate model simu- lations, Prasanna and Annamalai [2012] showed that dry advection is the principal moist process

The comparison of static stability (Figure 9) during SHEBA and N-ICE2015 reveals that the N-ICE2015 observa- tions over thinner, younger sea ice in the North Atlantic Arctic

The empirical coupling of the gov- erning transport parameters, i.e., the dependence of permeability and migration celerity on grain size and bottom water velocity, allows for

We analyze diurnal and seasonal cycles

The loading provided by such slow sediment deposition is neither rapid enough to cause significant excess pore pressure where overburden is high nor to induce enough fluid flow or

The preprocessing procedure can reduce the data volume per satellite pass by over 98% for full-resolution data or by :::, 84% for the lower-resolution data while the number