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First 488 results for ” A Farnsworth”

1. Changing European hydroclimate under a collapsed AMOC in the Community Earth System Model

   The Atlantic Meridional Overturning Circulation (AMOC) is expected to weaken or even collapse und...

   van Westen, R. M., van der Wiel, K., Falkena, S. K. J., and Selten, F. | Journal: Hydrol. Earth Syst. Sci. | Volume: 29 | Year: 2025 | doi: https://doi.org/10.5194/hess-29-6607-2025

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2. EARTH EXPLORER 11 CANDIDATE MISSION SEASTAR REPORT FOR ASSESSMENT

   Seastar is a new Earth Explorer mission concept dedicated to observing fast-evolving small-scale ...

   Christine Gommenginger. Aida Alvera-Azcarate, Ole Baltazar Andersen, Fabrice Ardhuin, Antonio Bonaduce, Øyvind Breivik, Fabrice Collard, Mohammed Dabboor, Robert King, Joanna Staneva, Ad Stoffelen, David Woolf | Year: 2023

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3. Isoprene emissions track the seasonal cycle of canopy temperature, not primary production: evidence from remote sensing

   Isoprene is important in atmospheric chemistry, but its seasonal emission pattern – especially in...

   PN Foster, M van Weele, et al. | Status: published | Journal: Biogeosciences | Volume: 11 | Year: 2014 | doi: 10.5194/bg-11-3437-2014

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4. Offshore wind climatology based on synergetic use of Envisat ASAR, ASCAT and QuikSCAT

   Highlights: • We combine satellite surface ocean wind vector data from three satellites. • Offsho...

   C Hasager, A Mouche, M Badger, F Bingol, I Karagali, T Driesenaar, A Stoffelen, A Pina, N Longepe | Status: published | Journal: Remote Sens. Environ. | Volume: 156 | Year: 2014 | First page: 247 | Last page: 263 | doi: doi:10.1016/j.rse.2014.09.030

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5. Role of synoptic- and meso-scales on the evolution of the boundary-layer wind profile over a coastal region: the near-coast diurnal acceleration

   The contributions of synoptic- and meso-scales to the boundary layer wind profile evolution in a ...

   PA Jiminez, J Vila-Guerau de Arellano, J Dudhia, FC Bosveld | Status: published | Journal: Meteor. Atmos. Phys. | Volume: 128 | Year: 2016 | First page: 39 | Last page: 56 | doi: 10.1007/s00703-015-0400-6

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