Preprints
https://doi.org/10.5194/acp-2021-1004
https://doi.org/10.5194/acp-2021-1004
 
13 Jan 2022
13 Jan 2022
Status: a revised version of this preprint was accepted for the journal ACP and is expected to appear here in due course.

Radiative closure and cloud effects on the radiation budget based on satellite and ship-borne observations during the Arctic summer research cruise PS106

Carola Barrientos-Velasco, Hartwig Deneke, Anja Hünerbein, Hannes J. Griesche, Patric Seifert, and Andreas Macke Carola Barrientos-Velasco et al.
  • Leibniz Institute for Tropospheric Research, Leipzig, Germany

Abstract. For understanding Arctic climate change, it is critical to quantify and address uncertainties in climate data records on clouds and radiative fluxes derived from long-term passive satellite observations. A unique set of observations collected during the research vessel Polarstern PS106 expedition (28 May to 16 July 2017) by the OCEANET facility is exploited here for this purpose and compared with the CERES SYN1deg Ed. 4.1 satellite remote sensing products. Mean cloud fraction (CF) of 86.7 % for CERES and 76.1 % for OCEANET were found for the entire cruise. The difference of CF between both data sets is due to different spatial resolution and momentary data gaps due to technical limitations of the set of ship-borne instruments. A comparison of radiative fluxes during clear-sky conditions enables radiative closure for CERES products by means of independent radiative transfer simulations. Several challenges were encountered to accurately represent clouds in radiative transfer under cloudy conditions, especially for ice-containing clouds and low-level stratus (LLS) clouds. During LLS conditions, the OCEANET retrievals were in particular compromised by the altitude detection limit of 155 m of the cloud radar. Radiative fluxes from CERES show a good agreement with ship observations, having a bias (standard deviation) of −6.0 (14.6) W m−2 and 23.1 (59.3) W m−2 for the downward longwave (LW) and shortwave (SW) fluxes, respectively. Based on CERES products, mean values of the radiation budget and the cloud radiative effect (CRE) were determined for the PS106 cruise track and the central Arctic region (70°–90° N). For the period of study, the results indicate a strong influence of the SW flux in the radiation budget, which is reduced by clouds leading to a net surface CRE of −8.8 W m−2 and −9.3 W m−2 along the PS106 cruise and for the entire Arctic, respectively. The similarity of local and regional CRE supports that the PS106 cloud observations can be considered to be representative of Arctic cloudiness during early summer.

Carola Barrientos-Velasco et al.

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on acp-2021-1004', Anonymous Referee #1, 31 Jan 2022
    • AC2: 'Reply on RC1', Carola Barrientos Velasco, 17 May 2022
  • RC2: 'Comment on acp-2021-1004', Anonymous Referee #2, 21 Feb 2022
    • AC1: 'Reply on RC2', Carola Barrientos Velasco, 17 May 2022
  • AC3: 'Comment on acp-2021-1004', Carola Barrientos Velasco, 13 Jun 2022

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on acp-2021-1004', Anonymous Referee #1, 31 Jan 2022
    • AC2: 'Reply on RC1', Carola Barrientos Velasco, 17 May 2022
  • RC2: 'Comment on acp-2021-1004', Anonymous Referee #2, 21 Feb 2022
    • AC1: 'Reply on RC2', Carola Barrientos Velasco, 17 May 2022
  • AC3: 'Comment on acp-2021-1004', Carola Barrientos Velasco, 13 Jun 2022

Carola Barrientos-Velasco et al.

Carola Barrientos-Velasco et al.

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Short summary
This article describes an intercomparison of radiative fluxes and cloud properties from satellite, ship-borne observations and 1D radiative transfer simulations. The analysis focuses on the period of the research expedition PS106 aboard the German research vessel Polarstern. The results are presented in detailed case studies, time-series for the PS106 cruise and extended to the Central Arctic region. The findings illustrate the main periods of agreement and discrepancies of both points of view.
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