Abstract

The radiation budget from surface observations and parameterizations is combined with that from satellite observations along the cruise tracks of the German icebreaker POLARSTERN in the North and South Atlantic under tropical, subtropical and mid-latitude conditions. Between 2008 and 2010 The German Leibniz-network OCEANET participated in six transfers from or to Bremerhaven, Germany to or from Punta Arenas, Southern Chile or Cape Town, South Africa. The present chapter introduces exemplarily the atmospheric measurements and resulting radiation products. The following properties are derived: Standard meteorological data, broadband downward solar and thermal irradiances, underwater profiles of spectral irradiance, latent and sensible heat fluxes, humidity and temperature profiles, water vapour and liquid water path, aerosol optical thickness and vertical profiles of aerosol optical thickness, cloud cover and cloud type. Cloud radiative effects at the surface have been determined for different marine cloud types. Together with top-of-atmosphere radiation fluxes from the SEVIRI radiometer onboard METEOSAT, the effect of clouds on atmospheric heating or cooling have been determined. The resulting cloud/radiation correlations will help to quantify the effects of clouds on the surface, ToA- and atmospheric radiation budget and to evaluate the ability of climate models to simulate these effects.

Highlights

  • Clouds are an impressive manifestation of complex dynamical-thermodynamical processes in the atmosphere

  • The aim of this chapter was to introduce the concept of the cloud radiative effect as an important driver of the energy budget of our climate system

  • Five years of data have been collected during the Atlantic Ocean transfer cruises of the Russian research vessels ACADEMICIAN IOFFE and ACADEMICIAN VAVILOV as well as the German research vessel POLARSTERN

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Summary

Introduction

Clouds are an impressive manifestation of complex dynamical-thermodynamical processes in the atmosphere. (Negative) latent heat is transported by cloud related condensation and evaporation processes, and the corresponding transports of fresh water determine vegetation over land and the stability of the oceanic boundary layer This well recognized significance of the cloudy atmosphere on the state of the earth’s climate stands in strong contrast to our quantitative understanding of the relevant physical processes in clouds. Regional and large-scale patterns of the energy budget produce the dynamical forcing for cloud evolution This complex interplay between clouds and energy budgets is recognised as the largest source for uncertainties in understanding climate processes [4]. A detailed description of all measurements performed during the OCEANET cruises can be found in the POLARSTERN cruise reports [7, 8]

Atmospheric measurement devices
Atmospheric composition
Cloud induced radiation enhancement
Radiation budget
Cloud radiative effect
Conclusions
Findings
IPCC 2007
Full Text
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