Skip to main content

and
  1. No Access

    Article

    The Wind Profile in the Coastal Boundary Layer: Wind Lidar Measurements and Numerical Modelling

    Traditionally it has been difficult to verify mesoscale model wind predictions against observations in the planetary boundary layer (PBL). Here we used measurements from a wind lidar to study the PBL up to 800...

    R. Floors, C. L. Vincent, S. -E. Gryning, A. Peña in Boundary-Layer Meteorology (2013)

  2. No Access

    Article

    Cross-Spectra Over the Sea from Observations and Mesoscale Modelling

    Cospectra and quadrature spectra are calculated for six pairs of tall offshore measurement masts near the Horns Rev I wind farm in the Danish North Sea and the Nysted wind farm in the Baltic sea. The mast-pair...

    C. L. Vincent, X. G. Larsén, S. E. Larsen, P. Sørensen in Boundary-Layer Meteorology (2013)

  3. No Access

    Article

    Response to nutrient enrichment by the plankton of Antarctic coastal lakes and the inshore Ross Sea

    Water samples from coastal lakes and ponds on Ross Island (77°S) and from the adjacent Ross Sea were analyzed to determine nutrient supply relative to the population size of planktonic algae and bacteria. An e...

    W. F. Vincent, C. L. Vincent in Polar Biology (1982)

  4. No Access

    Article

    Nitrous oxide cycling in Lake Vanda, Antarctica

    Nitrous oxide (N2O) is a key intermediate for several steps of the aquatic nitrogen cycle. In oxygenated oceanic waters, bacterial oxidation of amino- and ammonium-N is a dominant source of N2O (ref. 1); in regio...

    W. F. Vincent, M. T. Downes, C. L. Vincent in Nature (1981)