Daytime Low Stratiform Cloud Detection on AVHRR Imagery
Abstract
:1. Introduction
2. Characteristics of Low Stratiform Clouds
2.1. Physical Properties of Stratiform Clouds
2.2. Spectral Properties of Stratiform Clouds
3. Overview on Satellite Low Stratiform Cloud/Fog-Detection Algorithms
4. Input Data
4.1. Satellite Data
- NOAA16—with the channel 3b (3.7 μm) configuration and early morning overpass time (as for the year 2011), which has been changing due to the satellite orbital drift.
- NOAA17—with the channel 3a/3b (1.6/3.7 μm) configurations and morning overpass time.
- NOAA18—with the channel 3b (3.7 μm) configuration and midday overpass time.
4.2. Meteorological and Ancillary Data
- cloud types (at low, middle and high levels).
- present weather—coded values describing the current atmospheric conditions. Codes from 10–12 to 40–49 indicate different types of fog events.
5. Methodology of LSC Detection
5.1. Probabilistic Cloud Mask (PCM)
5.2. Algorithm Design
- 0.6 μm reflectance which contains information about the cloud optical depth.
- 1.6/3.7 μm reflectance which contains information about the cloud droplet radius.
- 10.8 μm BT which contains information about the thermodynamic state of a cloud.
- SKT-10.8 μm temperature difference which contains information about the cloud height.
- 10.8–12.0 μm BTD which indicates the presence of upper-level cloudiness.
- broken cloudiness flag (described in Section 5.3).
- SYNOP report indicates presence of the LSC.
- SYNOP report indicates absence of middle or high clouds (in case they could be visible through the inhomogeneous LSC cover).
- Thermal contrast between the 10.8 μm cloud top BT and the SKT does not exceed 18 K. This roughly corresponds to the cloud top height at 3 km assuming the temperature lapse rate of 0.6 K/100 m.
- 10.8 μm BT has to be greater than 232 K to exclude thick homogeneous cirrus clouds [53].
- 10.8–12.0 μm BTD has to be lower than 1 K to exclude high clouds.
- 0.6 μm reflectance has to be greater than 0.2 to exclude clouds with small optical thickness such as cirrus [54].
5.3. Preparation of Input Data
5.4. Algorithm Training Phase
5.5. Algorithm Validation and Derivation of LSC Data
6. Discussion of Acquired Results
6.1. Validation against SYNOP Observations
6.2. Spatial Distribution of LSC over Europe
6.3. Spatio-Temporal Distribution of LSC over Europe
7. Conclusions
- Within the SYNOP reports, LSC cannot be identified together with middle and/or high clouds.
- Thermal contrast between the 10.8 μm cloud top brightness temperature (BT) and skin surface temperature retrieved from a climate model cannot exceed 18 K.
- 10.8 μm BT has to be greater than 232 K.
- 10.8–12.0 μm BT difference has to be lower than 1 K.
- 0.6 μm reflectance has to be greater than 0.2.
Acknowledgments
Conflicts of Interest
- Author ContributionsPresented study was performed within the PhD dissertation of Jan Pawel Musial, who developed the proposed satellite LSC discrimination methodology. Fabia Hüsler and Christoph Neuhaus were responsible for preparation of AVHRR data, analysis of its integrity and quality assessment. Melanie Sütterlin and Stefan Wunderle were involved in structuring the research analyses, discussing its results, and correcting the manuscript.
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Code | Description |
---|---|
11 | cirrus fibratus or cirrus uncinus |
12 | cirrus spissatus, in patches or entangled sheaves |
13 | cirrus spissatus cumulonimbogenitus |
14 | cirrus uncinus or fibratus,or both, progressively invading the sky |
15–16 | cirrus (often in bands) and cirrostratus, or cirrostratus alone with the continuous veil |
17 | cirrostratus covering the whole sky |
18 | cirrostratus not progressively invading the sky and not entirely covering it |
19 | cirrocumulus alone, or cirrocumulus predominant among others high clouds |
21 | altostratus translucidus |
22 | altostratus opacus or nimbostratus |
23 | altocumulus translucidus at a single level |
24 | patches (often lenticularis) of altocumulus translucidus |
25 | altocumulus translucidus in bands, or layers of altocumulus translucidus or opacus |
26 | altocumulus cumulogenitus (or cumulonimbogenitus) |
27 | altocumulus translucidus or opacus, or altocumulus opacus in a single layer |
28 | altocumulus castellanus or flocus |
29 | altocumulus of chaotic sky, generally at several levels |
31 | cumulus humilis or cumulus fractus other than of bad weather, or both |
32 | cumulus mediocris or congestus |
33 | cumulonimbus calvus, with or without cumulus, stratocumulus or stratus |
34 | stratocumulus cumulogenitus |
35 | stratocumulus other than stratocumulus cumulogenitus |
36 | stratus nebulosus or stratus fractus other than of bad weather, or both |
37 | stratus fractus or cumulus fractus of bad weather usually below altostratus or nimbostratus |
38 | cumulus and stratocumulus other than stratocumulus cumulogenitus |
39 | cumulonimbus capillatus (often with an anvil) |
Code | Description |
---|---|
10 | mist |
11 | patches of shallow fog or ice fog at station |
12 | more or less continuous shallow fog or ice fog at station |
40 | fog or ice fog at a distance at the time of observation but not at station |
41 | fog or ice fog in patches |
42 | fog or ice fog, sky visible, has become thinner during the preceding hour |
43 | fog or ice fog, sky invisible, has become thinner during the preceding hour |
44 | fog or ice fog, sky visible, no appreciable change during the preceding hour |
45 | fog or ice fog, sky invisible, no appreciable change during the preceding hour |
46 | fog or ice fog, sky visible, has become thicker during the preceding hour |
47 | fog or ice fog, sky invisible, has become thicker during the preceding hour |
48 | fog depositing rime sky visible |
49 | fog depositing rime sky invisible |
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Musial, J.P.; Hüsler, F.; Sütterlin, M.; Neuhaus, C.; Wunderle, S. Daytime Low Stratiform Cloud Detection on AVHRR Imagery. Remote Sens. 2014, 6, 5124-5150. https://doi.org/10.3390/rs6065124
Musial JP, Hüsler F, Sütterlin M, Neuhaus C, Wunderle S. Daytime Low Stratiform Cloud Detection on AVHRR Imagery. Remote Sensing. 2014; 6(6):5124-5150. https://doi.org/10.3390/rs6065124
Chicago/Turabian StyleMusial, Jan Pawel, Fabia Hüsler, Melanie Sütterlin, Christoph Neuhaus, and Stefan Wunderle. 2014. "Daytime Low Stratiform Cloud Detection on AVHRR Imagery" Remote Sensing 6, no. 6: 5124-5150. https://doi.org/10.3390/rs6065124
APA StyleMusial, J. P., Hüsler, F., Sütterlin, M., Neuhaus, C., & Wunderle, S. (2014). Daytime Low Stratiform Cloud Detection on AVHRR Imagery. Remote Sensing, 6(6), 5124-5150. https://doi.org/10.3390/rs6065124