2022
DOI: 10.5194/acp-22-9537-2022
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Observations of cold-cloud properties in the Norwegian Arctic using ground-based and spaceborne lidar

Abstract: Abstract. The role of clouds in the surface radiation budget is particularly complex in the rapidly changing Arctic. However, despite their importance, long-term observations of Arctic clouds are relatively sparse. Here, we present observations of cold clouds based on 7 years (2011–2017) of ground-based lidar observations at the Arctic Lidar Observatory for Middle Atmosphere Research (ALOMAR) in Andenes in the Norwegian Arctic. In two case studies, we assess (1) the agreement between a co-located cirrus cloud … Show more

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Cited by 3 publications
(3 citation statements)
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“…They report average cirrus cloud depths of 2.1 km during winter with a cloud base around 7.1 km and a cloud top on average at 9.3 km. Finally, Schäfer et al, (2022) use a ground based and space-born lidar and measure cirrus clouds over the Norwegian arctic for a period of seven years. They find a yearly average cloud thickness of 2.2 km, an average cloud base at 6.9 km and cloud top at 9.1 km.…”
Section: Discussionmentioning
confidence: 99%
“…They report average cirrus cloud depths of 2.1 km during winter with a cloud base around 7.1 km and a cloud top on average at 9.3 km. Finally, Schäfer et al, (2022) use a ground based and space-born lidar and measure cirrus clouds over the Norwegian arctic for a period of seven years. They find a yearly average cloud thickness of 2.2 km, an average cloud base at 6.9 km and cloud top at 9.1 km.…”
Section: Discussionmentioning
confidence: 99%
“…where Nb is the number of sky background photons received by each pulse; Pb is the sky background radiation intensity (W•m −2 •sr −1 •nm −1 ), and for a 532 nm wavelength, it is generally believed Pb = 0.2 W•m −2 •sr −1 •nm −1 in the daytime; θ is the viewing angle of the telescope (mrad); d ωl is filter bandwidth (nm); A r is the receiving area of the telescope (m 2 ); T r is the optical transmittance of the lidar receiving optical unit; ∆t is the time resolution (s) of the lidar. According to Equation (10), factors affecting the intensity of the sky background radiation signal received by the lidar are also composed of three parts.…”
Section: Simulation Of Background Signal and Noise Of Spaceborne Lidarmentioning
confidence: 99%
“…Therefore, it is of positive significance to study the spatial distribution and change process of clouds and aerosols for improving the precision of weather forecast and predicting global climate change [6][7][8][9]. In order to realize the real-time dynamic monitoring of global clouds and aerosols, spaceborne lidar remote sensing has become a hotspot of environmental surveillance research [10][11][12][13]. However, due to the limitation of the orbit and operation mechanism, the measurement data of a single spaceborne lidar cannot accurately describe atmospheric conditions, so it is necessary to adopt other technical means and build the lidar surveillance network to improve the precision of detection.…”
Section: Introductionmentioning
confidence: 99%