Influence of the ice growth rate on the incorporation of gaseous HCl

o ff sets between di ff erent surface types and small thermal o ff sets in general (exclud- ing wetlands and peat), (ii) a clear influence of the micro-topography at wind exposed

nections, (2) connections can be significantly di ff erent for di ff erent threshold levels, (3) there is generally an inverse relationship between the clustering coe ffi cient and

it thus seems pivotal (i) to assess the contribution of the di ff erent components of the growth response, particularly the duration of the favorable period of growth and the

The purposes of this paper are: (1) to investigate the e ff ect of di ff erent scenarios of antecedent soil moisture organisation on the runo ff in a distributed hydrologic model at

These consistent decreases in decay rate (using three di ff erent isotopes) during two di ff er- ent solar eclipses can only be explained by the mass of the Moon and the mass of

Next, we calculate the temporal correlation between di ff erent latitudes of timeseries of annual and 5-daily volume transports and their Ekman and geostrophic components, in

simulations are utilized to explain and explore di ff erences in the soil moisture response due to di ff erent vegetation types and their impact on the temporal variability of

To establish the extent to which a snow cover will mitigate the albedo e ff ect of black carbon in sea ice two di ff erent Arctic snow types (also described by Grenfell and