Aarhus University Seal / Aarhus Universitets segl

Observed and modelled cloud cover up to 6 km height at Station Nord in the high Arctic

New publication by Sven‐Erik Gryning, Ekaterina Batchvarova, Rogier Floors, Christoph Münkel, Henrik Skov, Lise Lotte Sørensen

2021.03.30 | Peter Schmidt Mikkelsen

Abstract:

We present results from an analyses of cloud cover based on profiles of the attenuated backscatter coefficient from an 8‐year‐long data series (July 2011–April 2019). The observations are carried out in the high Arctic by a ceilometer with a maximum range setting of 7.7 km from the Villum Research Station at Station Nord, Greenland. Results show that the hourly cloud cover turned out to follow a U‐shaped rather than Gaussian‐like distribution. Annual and seasonal cloud cover variation is illustrated. The cloud cover is larger during the autumn and winter as compared to summer and spring. The cloud cover exhibits a substantial variation from year to year without a clear trend. The cloud cover during spring is low and decreasing between 2012 and 2017. The cloud cover during the autumn of 2016 is lowest compared to the other years. The observed cloud cover is compared to the cloud cover provided in the ERA5 reanalysis dataset. The cloud cover for low clouds and medium clouds are combined to represent a total height of 6 km. Both the observed and modelled cloud cover is larger during winter as compared to summer‐time cloud cover. The measured reduction in the cloud cover for the autumn of 2016 is present in the reanalysis data as well but the measured low cloud cover during spring is not apparent in the reanalysis data. Because the cloud cover distribution is U‐shaped rather than of a Gaussian nature, standard metrics are not applicable. We apply a generalized skill score that is developed for contingency tables or joint histograms. Three skill scores were calculated. It was found that for all three methods, skills for the predictability of the cloud cover by the ERA5 modelling is better for winter than summer and is poor during the spring.

doi.org/10.1002/joc.6894

Arctic Research Centre