Abstract
Abstract. This study presents and evaluates several candidate approaches for downscaling observations from the Spinning Enhanced Visible and Infrared Imager (SEVIRI) in order to increase the horizontal resolution of subsequent cloud optical thickness (τ) and effective droplet radius (reff) retrievals from the native ≈3km×3km spatial resolution of the narrowband channels to ≈1km×1km. These methods make use of SEVIRI's coincident broadband high-resolution visible (HRV) channel. For four example cloud fields, the reliability of each downscaling algorithm is evaluated by means of collocated 1 km×1 km MODIS radiances, which are reprojected to the horizontal grid of the HRV channel and serve as reference for the evaluation. By using these radiances, smoothed with the modulation transfer function of the native SEVIRI channels, as retrieval input, the accuracy at the SEVIRI standard resolution can be evaluated and an objective comparison of the accuracy of the different downscaling algorithms can be made. For the example scenes considered in this study, it is shown that neglecting high-frequency variations below the SEVIRI standard resolution results in significant random absolute deviations of the retrieved τ and reff of up to ≈14 and ≈6 µm, respectively, as well as biases. By error propagation, this also negatively impacts the reliability of the subsequent calculation of liquid water path (WL) and cloud droplet number concentration (ND), which exhibit deviations of up to ≈89gm-2 and ≈177cm-3, respectively. For τ, these deviations can be almost completely mitigated by the use of the HRV channel as a physical constraint and by applying most of the presented downscaling schemes. Uncertainties in retrieved reff at the native SEVIRI resolution are smaller, and the improvements from downscaling the observations are less obvious than for τ. Nonetheless, the right choice of downscaling scheme yields noticeable improvements in the retrieved reff. Furthermore, the improved reliability in retrieved cloud products results in significantly reduced uncertainties in derived WL and ND. In particular, one downscaling approach provides clear improvements for all cloud products compared to those obtained from SEVIRI's standard resolution and is recommended for future downscaling endeavors. This work advances efforts to mitigate impacts of scale mismatches among channels of multiresolution instruments on cloud retrievals.
Highlights
In studies of the role of clouds in the climate system, the bispectral solar reflective method described by Twomey and Seton (1980), Nakajima and King (1990), and Nakajima et al (1991) is widely used to infer cloud optical and physical properties from satellite-based sensors
This study presents and evaluates several candidate approaches for downscaling observations from the Spinning Enhanced Visible and Infrared Imager (SEVIRI) in order to increase the horizontal resolution of subsequent cloud optical thickness (τ ) and effective droplet radius retrievals from the native ≈ 3 km × 3 km spatial resolution of the narrowband channels to ≈ 1 km × 1 km
The aim of this paper is to critically evaluate several candidate approaches for downscaling of the SEVIRI narrow-band reflectances for operational usage and to identify the most promising of these schemes, exploiting the fact that information on small-scale variability is available from its broadband high-resolution visible (HRV) channel
Summary
In studies of the role of clouds in the climate system, the bispectral solar reflective method described by Twomey and Seton (1980), Nakajima and King (1990), and Nakajima et al (1991) is widely used to infer cloud optical and physical properties from satellite-based sensors. Based on observations of solar reflectance (r) from a channel pair at wavelengths with conservative scattering (usually around 0.6 or 0.8 μm) and significant absorption by cloud droplets (common channels are 1.6, 2.2, and 3.7 μm), respectively, this method simultaneously estimates the cloud optical depth (τ ) and effective droplet radius (reff) of a sampled cloudy pixel. This method relies on a number of assumptions which are often violated in nature: clouds are considered to be horizontally homogeneous and to have a prescribed ver-. The observed cloud top reflectance field is usually described by one-dimensional (1-D) plane-parallel radiative transfer, which neglects horizontal photon transport between neighboring atmospheric columns
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