a Ghent University, Faculty of Bioscience Engineering, Department of Agricultural Economics, Coupure Links 653, 9000 Ghent, Belgium b Ghent University, Faculty of Bioscience Engineering, Laboratory of Tropical and Subtropical Agronomy and Ethnobotany, Coupure Links 653, 9000 Ghent, Belgium c World Agroforestry Centre, West and Central African Region (ICRAF-WCA), PO Box 16317 Yaounde, Cameroon d...

1 Facultad de Ciencias Químicas, Universidad Autónoma de San Luis Potosí. Av. Dr. Manuel Nava 6, Zona Universitaria. 78210 San Luis Potosí San Luis Potosí México. [email protected] 2 Institute for Technology and Resources Management in the Tropics and Subtropics, Cologne University of Applied Sciences. 3 Agenda Ambiental, Universidad Autónoma de San Luis Potosí. exploring mexican adolescen...

Mesospheric water vapour measurements taken by the SMR instrument onboard the Odin satellite between 2002 and 2006 have been analysed with focus on the meso-spheric semi-annual circulation in the tropical and subtropical region. This analysis provides the first complete picture of mesospheric SAO in water vapour, covering alti-5 tudes above 80 km where the only previous study based on UARS/HALO...

Improved estimates of the radiative forcing from tropospheric ozone increases since the preindustrial have been calculated with the tropospheric chemistry model used at the Goddard Institute for Space Studies (GISS) within the GISS general circulation model (GCM). The chemistry in this model has been expanded to include simplified representations of peroxyacetylnitrates and non-methane hydrocar...

The development of a particular wintertime atmospheric circulation regime over the North Atlantic, comprising a northward shift of the North Atlantic eddy-driven jet stream and an associated strong and persistent ridge in the subtropics, is investigated. Several different methods of analysis are combined to describe the temporal evolution of the events and relate it to shifts in the phase of th...

About a quarter of the total anthropogenic CO2 emissions during industrial era has been absorbed by ocean. The rate limiting step for this uptake is transport carbon (Cant) from ocean mixed layer where it to interior stored. While generally known that deep water formation sites are important vertical transport, exact magnitude fluxes across base in different regions uncertain. Here, we determin...