Combination of Spectral and Textural Features in the MSG Satellite Remote Sensing Images for Classifying Rainy Area into Different Classes
- 129 Downloads
Abstract
The rainfall intensity classification technique using spectral and textural features from MSG/SEVIRI (Meteosat Second Generation/Spinning Enhanced Visible and Infrared) satellite data is proposed in this paper. The study is carried out over north of Algeria. The developed method is based on the artificial neural multilayer perceptron network (MLP). Two MLP algorithms are used: the MLP-S based only on spectral parameters and the MLP-ST that use both spectral and textural features. The MLP model is created with three layers (input, hidden, and output) that consist of 6 output neurons in the output layer that represent the 6 rain intensities classes: very high, moderate to high, moderate, light to moderate, light and no rain and 10 spectral input neurons for the MLP-S and 15 input neurons for MLP-ST, which as ten spectral features that were calculated from MSG thermal infrared brilliance temperature and brilliance temperature difference and as five textural features, and The rainfall intensity areas classified by the proposed technique are validated against ground-based radar data. The rainfall rates used in the training set are derived from Setif radar measurements (Algeria). The results obtained after applying this method show that the introduction of textural parameters as additional information works in improving the classification of different rainfall intensities pixels in the MSG/SEVIRI imagery compared to the techniques based only on spectral information. These results are compared with results obtained with the probability of rainfall intensity (PRI). This comparison revealed a clear outperformance of the MLP algorithms over the PRI algorithms. Best results are provided by the MLP-ST algorithm. The combination of spectral and textural features in the MSG–SEVIRI imagery is important and for the classification of the rainfall intensities to different classes.
Keywords
Image classification Satellite and radar data Spectral and textural features Rainfall intensities Artificial neural networkReferences
- Adler, R. F., & Mack, R. A. (1984). Thunderstorm cloud height rainfall rate relations for use with satellite rainfall estimation techniques. Journal of Climate and Applied Meteorology, 23, 280–296.CrossRefGoogle Scholar
- Adler, R. F., & Negri, A. J. (1988). A satellite technique to estimate tropical convective and stratiform rainfall. Journal of Applied Meteorology, 27, 30–51.CrossRefGoogle Scholar
- Amadasun, M., & King, R. (1989). Textural features corresponding to textural properties. IEEE Transactions on Systems, Man, and Cybernetics, 19(5), 1264–1274.CrossRefGoogle Scholar
- Ameur, Z., Ameur, S., Adane, A., Sauvageot, H., & Bara, K. (2004). Cloud classification using the textural features of Meteosat images. International Journal of Remote Sensing, 25, 4491–4503.CrossRefGoogle Scholar
- Aminou, D. M. A. (2002). MSG’s SEVIRI instrument. ESA Bulletin, 111, 15–17.Google Scholar
- Anagnostou, E. N., & Kummerow, C. (1997). Stratiform and convective classification of rainfall using SSM/I 85-GHz brightness temperature observations. Journal of Atmospheric and Oceanic Technology, 14, 570–575.CrossRefGoogle Scholar
- Arkin, P. A., & Meisner, B. N. (1987). The relationship between large-scale convective rainfall and cold cloud over the western hemisphere during 1982–1984. Monthly Weather Review, 115, 51–74.CrossRefGoogle Scholar
- Baraldi, A., & Parmiggiani, F. (1999). An Investigation of the textural characteristics associated with gray level co-occurence matrix statistical parameters. IEEE Transactions on Geoscience and Remote Sensing, 33, 293–304.CrossRefGoogle Scholar
- Bendix, J., Reudenbach, J. C., & Rollenbeck, R. (2003). The Marburg Satellite Station. In Proceedings of the 2002 Meteorological Satellite Users’ Conference. Dublin, EUMETSAT, pp. 139–146.Google Scholar
- Cocquerez, J. P., & Philipp, S. (1995). Analyse d’images: Filtrage et segmentation. Paris: Masson.Google Scholar
- Connors, R. W., Trivedi, M. H., & Harlow, C. A. (1984). Segmentation of a high resolution urban scene using texture operators. Compact Graphics Image Processing, 25, 273–310.CrossRefGoogle Scholar
- Curic, M., & Janc, D. (2011). Analysis of predicted and observed accumulated convective precipitation in the area with frequent split storms. Hydrology and Earth System Sciences, 15, 3651–3658.CrossRefGoogle Scholar
- Ebert, E. E., & Manton, M. J. (1998). Performance of satellite rainfall estimation algorithms during TOGA COARE. Journal of the Atmospheric Sciences, 55, 1538–1557.CrossRefGoogle Scholar
- EUMETSAT. (2008). Applications of Meteosat Second Generation-conversion from counts to radiances and from radiances to rightness temperatures and reflectance. http://oiswww.eumetsat.org/WEBOPS/msg_interpretation/index.html
- Feidas, H. (2011). Study of a mesoscale convective complex over the eastern Mediterranean basin with Meteosat data. In Eumetsat Meteorological Satellite Conference, Oslo, Norway, 5–9 September, 2011.Google Scholar
- Feidas, H., & Giannakos, A. (2010). Identifying precipitating clouds in Greece using multispectral infrared Meteosat Second Generation satellite data. Theoretical and Applied Climatology. doi: 10.1007/s00704-010-0316-5.Google Scholar
- Feidas, H., & Giannakos, A. (2012). Classifying convective and stratiform rain using multispectral infrared Meteosat Second Generation satellite data. Theoretical and Applied Climatology, 108(3), 613–630.CrossRefGoogle Scholar
- Freeman, J. A., & Skapura, D. M. (1991). Neural networks: Algorithms, applications, and programming techniques. Reading: Addison-Wesley.Google Scholar
- Fritz, S., & Laszlo, I. (1993). Detection of water vapor in the stratosphere over very high clouds in the tropics. Journal Geophysical Research, 98(D12), 22959–22967.CrossRefGoogle Scholar
- Galushkin, A. I. (1997). Neural networks theory (pp. 368–375). Berlin: Springer. ISBN 978-3-540-48124-9.Google Scholar
- Haralick, R. M., Shanmugam, K., & Dinstein, I. (1973). Textural features for image classification. IEEE Transactions on Systems, Man and Cybernetics, 3(6), 610–621.CrossRefGoogle Scholar
- Hong, Y., Hsu, K., Sorooshian, S., & Gao, X. (2004). Precipitation estimation from remotely sensed imagery using an artificial neural network cloud classification system. Journal of Applied Meteorology, 43, 1834–1852.CrossRefGoogle Scholar
- Hong, Y., Kummerow, C. D., & Olson, W. S. (1999). Separation of convective and stratiform precipitation using microwave brightness temperature. Journal of Applied Meteorology, 38, 1195–1213.CrossRefGoogle Scholar
- Houze, R. L. (1997). Stratiform precipitation in regions of convection: A meteorological paradox. Bulletin of the American Meteorological Society, 78, 2179–2196.CrossRefGoogle Scholar
- Inoue, T. (1987a). A cloud type classification with NOAA-7 split window measurements. Journal Geophysical Research, 92, 3991–4000.CrossRefGoogle Scholar
- Inoue, T. (1987b). An instantaneous delineation of convective rainfall areas using split window data of NOAA-7 AVHRR. Journal of the Meteorological Society of Japan, 65, 469–481.CrossRefGoogle Scholar
- Inoue, T., Wu, X., & Bessho, K. (2001). Life cycle of convective activity in terms of cloud type observed by split window. In 11th Conference on Satellite Meteorology and Oceanography, Madison, WI, USA.Google Scholar
- Kaur, R., & Ganju, A. (2008). Cloud classification in NOAA AVHRR imageries using spectral and textural features. Journal of the Indian Society of Remote Sensing, 36, 167–174.CrossRefGoogle Scholar
- Kayitakire, F., Giot, P., & Defourny, P. (2002). Discrimination automatique de peuplements forestiers à partir d’orthophotos numériques couleur : un cas d’étude en Belgique. Journal canadien de télédétection, 28(5), 629–640.Google Scholar
- Kwon, E., Sohn, B., Schmetz, J., & Wats, P. (2010). Intercomparison of height assignment methods for opaque clouds over the tropics. Journal of the Atmospheric Sciences, 46(1), 11–19.Google Scholar
- Lamei, N., Hutchison, K. D., & Crawford, M. M. (1994). Cloud-type discrimination via multispectral textural analysis. Optical Engineering, 33, 1303–1313.CrossRefGoogle Scholar
- Laws, K. I. (1980). Rapid texture identification. SPIE, 238, 376–380.Google Scholar
- Lazri, M., Ameur, Z., Ameur, S., Mohia, Y., Brucker, J. M., & Testud, J. (2013a). Rainfall estimation over a Mediterranean region using a method based on various spectral parameters of SEVIRIMSG. Advances in Space Research. doi: 10.1016/j.asr.2013.07.036.Google Scholar
- Lazri, M., Ameur, S., Brucker, J. M., Testud, J., Hamadache, B., Hameg, S., Ouallouche, F., Mohia, Y. (2013b). Identification of raining clouds using a method based on optical and microphysical cloud properties from Meteosat Second Generation daytime and nighttime data. Applied Water Science. doi: 10.1007/s13201-013-0079-0.Google Scholar
- Levizzani, V. (2003). Satellite rainfall estimates: new perspectives for meteorology and climate from the EURAINSAT project. Annales Geophysicae, 46(2), 363–372.Google Scholar
- Levizzani, V., Schmetz, J., Lutz, H. J., Kerkmann, J., Alberoni, P. P., & Cervino, M. (2001). Precipitation estimations from geostationary orbit and prospects for Meteosat Second Generation. Meteorological Applications, 8, 23–41.CrossRefGoogle Scholar
- Lutz, H.-J., Inoue, T., & Schmetz, J. (2003). Notes and correspondence comparison of a split-window and a multi-spectral cloud classification for MODIS observations. Journal of the Meteorological Society of Japan, 81(3), 623–631.CrossRefGoogle Scholar
- Mecikalski, J. R., & Bedka, K. M. (2006). Forecasting convective initiation by monitoring the evolution of moving cumulus in daytime GOES imagery. Monthly Weather Review, 134, 49–68.CrossRefGoogle Scholar
- Mecikalski, J. R., Bedka, K. M., Mackenzie, W. M., & Simon, J. P. (2007). Convective initiation and lightning prediction: The potential of the MTG-FC imagery mission, Atmospheric Science Department, University of Alabama in Huntsville. In Cooperative Institute for Meteorological Satellite Studies University of Wisconsin-Madison Meteorological Satellite Conference, Amsterdam, The Netherlands, pp. 24–28Google Scholar
- Narasimha Rao, P. V., Sesha Sai, M. V. R., Sreenivas, K., Krishna Rao, M. V., Rao, B. R. M., Dwivendi, R. S., Venkataratnam, I. (2002). Textural analyses of IRS-ID panchromatic data for land cover classification. International Journal of Remote Sensing, 23(17), 3327–3345.CrossRefGoogle Scholar
- Nauss, T., & Kokhanovsky, A. A. (2006). Discriminating raining from non-raining clouds at mid-latitudes using multispectral satellite data. Atmospheric Chemistry and Physics, 6, 5031–5036.CrossRefGoogle Scholar
- Reudenbach, C., Nauss, T., & Bendix, J. (2007). Retrieving precipitation with GOES, Meteosat and Terra/MSG at the tropics and mid-latitudes. In V. Levizzani, P. Bauer, & F. J. Turk (Eds.), Measuring precipitation form space—Advances in global change research (Vol. 28). Netherlands: Springer.Google Scholar
- Rosenberger, C. (1999). Mise en oeuvre d’un système adaptatif de segmentation d’images. Thèse de l’université de Rennes 1.Google Scholar
- Sali, E., & Wolfson, H. (1992). Texture classification in aerial photographs and satellite data. International Journal of Remote Sensing, 13(18), 3395–3408.CrossRefGoogle Scholar
- Schmetz, J., Pili, P., Tjemkes, S., Just, D., Kerkmann, J., Rota, S., Ratier, A. (2002). An introduction to Meteosat Second Generation (MSG). Bulletin of the American Meteorological Society, 83, 977–992.CrossRefGoogle Scholar
- Schmetz, J., Tjemkes, S., Gube, M., & Van De Berg, L. (1997). Monitoring deep convection and convective overshooting with Meteosat. Advances in Space Research, 19, 433–441.CrossRefGoogle Scholar
- Shou, Y., Li, S., Shou, S., & Zhao, Z. (2006). Application of a cloud-texture analysis scheme to the cloud cluster structure recognition and rainfall estimation in a mesoscale rainstorm process. Advances in Atmospheric Sciences, 23(5), 767–774.CrossRefGoogle Scholar
- Simpson, J., Adler, R. F., & North, G. (1998). A proposed Tropical Rainfall Measurement Mission (TRMM) satellite. Bulletin of the American Meteorological Society, 69, 278–295.CrossRefGoogle Scholar
- Skapura, D. M. (1995). Building neural networks (pp. 31–32). Reading: Addison-Wesley Publishing Company.Google Scholar
- Strabala, K. I., Ackerman, S. A., & Menzel, W. P. (1994). Cloud properties inferred from 8–12 micron data. Journal of Applied Meteorology, 33(2), 212–229.CrossRefGoogle Scholar
- Thies, B., Nauss, T., & Bendix, J. (2008a). Discriminating raining from non-raining cloud areas at mid-latitudes using Meteosat Second Generation SEVIRI night-time data. Meteorological Applications. doi: 10.1002/met.56.Google Scholar
- Thies, B., Nauss, T., & Bendix, J. (2008b). Discriminating raining from non-raining cloud areas at mid-latitudes using Meteosat Second Generation SEVIRI day-time data. Atmospheric Chemistry and Physics, 8, 1–9.CrossRefGoogle Scholar
- Thies, B., Nauss, Τ., & Bendix, J. (2008c). Precipitation process and rainfall intensity differentiation using Meteosat Second Generation Spinning Enhanced Visible and Infrared Imager data. Geophysical Research, 113, D23206. doi: 10.1029/2008JD010464.CrossRefGoogle Scholar
- Tremblay, A. (2005). The stratiform and convective components of surface precipitation. Journal of the Atmospheric Sciences, 62, 1513–1528.CrossRefGoogle Scholar
- Weszka, J. S., Dyer, C. R., & Rosenfeld, A. (1976). A comparative study of texture measures for terrain classification. IEEE Transaction on Systems, Man and Cybernetics, SMC-6.Google Scholar