Circumpolar measurements of speciated mercury, ozone and carbon monoxide in the boundary layer of the Arctic Ocean

Altitude profiles further illustrate the confinement of ozone depletion and bromine en- hancement to the MBL. The WP-3D measurements shown in Fig. 7 illustrate that all

The origin of these differences between the two cruises has been investigated using back trajectory simulations and also, in the case of the summer cruise, the AMCOTS box

Impacts of sea-ice reduction on the future projection of pH and aragonite saturation values in the Arctic surface waters have been investigated by comparing the rates of

The very high RGM concentrations at both coastal sites could be influenced by the local production of oxidized gaseous mercury species over the Antarctic continent or by shelf

Concentration maxima of volatile organic iodine compounds in the bottom layer water and the cold, dense water over the Chukchi Sea in the western Arctic Ocean: a possibility

Because boundary layer height is di ffi cult to determine under stable Arctic conditions, (Ander- son and Ne ff , 2008) an error in the estimation of z e ff from the boundary

The sheer size of the Canadian Arctic, combined with the unique and dynamic nature of phytoplankton communities at widespread SCM, demonstrates the need to adapt ecosystem models

Using a vortex-edge definition based on the location of the steepest gradient in po- tential vorticity the vortex-averaged ozone depletion for the Arctic winter and spring 2002/2003