Abstract

Abstract. Cirrus clouds remain one of the key uncertainties in atmospheric research. To better understand the properties and physical processes of cirrus clouds, accurate large-scale observations from satellites are required. Artificial neural networks (ANNs) have proved to be a useful tool for cirrus cloud remote sensing. Since physics is not modelled explicitly in ANNs, a thorough characterisation of the networks is necessary. In this paper the CiPS (Cirrus Properties from SEVIRI) algorithm is characterised using the space-borne lidar CALIOP. CiPS is composed of a set of ANNs for the cirrus cloud detection, opacity identification and the corresponding cloud top height, ice optical thickness and ice water path retrieval from the imager SEVIRI aboard the geostationary Meteosat Second Generation satellites. First, the retrieval accuracy is characterised with respect to different land surface types. The retrieval works best over water and vegetated surfaces, whereas a surface covered by permanent snow and ice or barren reduces the cirrus detection ability and increases the retrieval errors for the ice optical thickness and ice water path if the cirrus cloud is thin (optical thickness less than approx. 0.3). Second, the retrieval accuracy is characterised with respect to the vertical arrangement of liquid, ice clouds and aerosol layers as derived from CALIOP lidar data. The CiPS retrievals show little interference from liquid water clouds and aerosol layers below an observed cirrus cloud. A liquid water cloud vertically close or adjacent to the cirrus clearly increases the average retrieval errors for the optical thickness and ice water path, respectively, only for thin cirrus clouds with an optical thickness below 0.3 or ice water path below 5.0 g m−2. For the cloud top height retrieval, only aerosol layers affect the retrieval error, with an increased positive bias when the cirrus is at low altitudes. Third, the CiPS retrieval error is characterised with respect to the properties of the investigated cirrus cloud (ice optical thickness and cloud top height). On average CiPS can retrieve the cirrus cloud top height with a relative error around 8 % and no bias and the ice optical thickness with a relative error around 50 % and bias around ±10 % for the most common combinations of cloud top height and ice optical thickness. Similarities with physically based retrieval methods are evident, which implies that even though the retrieval methods differ in the implementation of physics in the model, the retrievals behave similarly due to physical constraints. Finally, we also show that the ANN retrievals have a low sensitivity to radiometric noise in the SEVIRI observations. For optical thickness and ice water path the relative uncertainty due to noise is less than 10 % down to sub-visual cirrus. For the cloud top height retrieval the uncertainty due to noise is around 100 m for all cloud top heights.

Highlights

  • Cirrus clouds remain one of the key uncertainties in atmospheric research (e.g. Waliser et al, 2009; Eliasson et al, 2011; Stevens and Bony, 2013)

  • For this study (Sect. 4.3–4.6) we use a dataset of collocated CiPS input data (SEVIRI, ECMWF and auxiliary data; see Sect. 3.2) and cirrus properties retrieved by CALIOP (CTH, ice optical thickness (IOT), ice water path (IWP) and opacity information), allowing us to apply CiPS and compare the retrievals with the corresponding reference retrievals by CALIOP

  • Exploiting the information from nearby SEVIRI pixels using the regional maximum and regional average temperatures is clearly helpful in all aspects; their relative importance is comparable to the relative importance of Tsurf for the CTHCiPS, IOTCiPS and IWPCiPS retrievals, for example

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Summary

Introduction

Cirrus clouds remain one of the key uncertainties in atmospheric research (e.g. Waliser et al, 2009; Eliasson et al, 2011; Stevens and Bony, 2013). Strandgren et al (2017) exploit the main idea of Kox et al (2014) and combine four ANNs trained with SEVIRI thermal observations, model data and CALIOP products for the detection of thin cirrus clouds and the retrieval of the corresponding CTH, IOT and ice water path (IWP) along with an additional opacity information. The active CALIOP lidar provides vertical profiles of ice cloud extinction and makes use of polarisation to distinguish between liquid water and ice. The CiPS algorithm exploits the brightness temperatures of the Earth sensed by the passive imager SEVIRI to detect ice clouds and derive their optical and physical properties.

SEVIRI
CALIOP
Collocation dataset
Artificial neural networks
Characterisation of CiPS
Validation metrics
Relative importance of the CiPS input data
The CiPS retrieval accuracy for different surface types
Surface type classes from MODIS
Cirrus cloud detection
Cirrus cloud properties
The CiPS retrieval accuracy for different vertical cloud–aerosol structures
Vertical cloud–aerosol structures from CALIOP
Cirrus above aerosol layer C4 Cirrus adjacent to water cloud
Noise sensitivity analysis of CiPS
Perturbing the SEVIRI brightness temperatures
Noise sensitivity of CiPS
Findings
Conclusions
Full Text
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