Postglacial paleoceanography of central Baffin Bay from palynological tracers

The minimum values of freshwater palynomorph fluxes in our record during AD 1855–1900 ( ∼ 30 specimens cm −2 yr −1 ), coupled with the relatively high sea-surface tempera-

Figure 10: (A, B, C) Distribution of SMOS SSS minus S insitu without correction (black line) and with correction (dashed line) for the different study areas and for the whole

On both occasions that the N-ICE2015 camp drifted over the Atlantic Water inflow in winter, a storm was ongoing resulting in ocean-ice heat fluxes of 30 W m −2 due to the combined

The mixed layer in the Arctic Ocean is composed of cold and fresh waters, close to the freezing temperature, called the Polar Surface Water (Figure 1.9).. In the Canadian Basin,

1 depicts the time required for a four-faced MPAR to complete a specific convective weather volume scan, based on the fraction of the radar’s scan-time allocated to

We illustrate the influence of the Ring wavelength dependence on DOAS measurements using zenith sky and direct sun spectra acquired on 21 July when the aerosol loading was

While there has been much work examining the affects of social network structure on innovation adoption, models to date have lacked im- portant features such as

Des planchers composite bois-béton renforcés avec des armatures font l’objet de test de flexion 4 points afin de caractériser leur comportement mécanique à