Abstract
One of the most extreme climatic occurrences, drought is distinct from other climatic phenomena in that it can happen at any time and in all climatic zones while also varying greatly from one area to another. Farmers in the region encounter considerable temporal and spatial variability in water supply during cropping seasons with frequent and longer dry spells. Agricultural drought is typical in dry land. Therefore, spatio-temporal variation in agricultural drought identification is important for policy maker as well planner. To examine the moisture surplus and deficit of the soil to crop, drought year has been estimated using Standardized Precipitation Index (SPI) 6 with the help of monthly precipitation of 116 years data. Seasonal “Land Surface Temperature (LST) and Normalized Difference Vegetation Index (NDVI) have been estimated to derive three other indices: Vegetation Condition Index (VCI), Temperature Condition Index (TCI), and Vegetation Health Index”. The multispectral band ratios have been performed to evaluate vegetation density and vegetation health to assess drought conditions over the study area (VHI). In order to determine the VHI of the study area for this paper, four years (1990, 2000, 2010, and 2017) were selected, out of which two experienced the severe drought (2000 and 2010).In the year of 1990 VHI value expressed that drought condition of this study area was ranges between moderate droughts to mild droughts but on the other hand in 2017 it fall in the category of severe drought (Below 20 VHI value). The four-year analysis period’s findings indicated that the sample block is currently facing a moderate to severe drought situation.
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References
Aghakouchak, A., Farahmand, A., Melton, F., Teixeira, J., Anderson, M., Wardlow, B., & Hain, C. (2015). Remote sensing of drought: Progress, challenges and opportunities. Reviews of Geophysics, 53.
Agnew, C. T., & Chappell, A. (2000). Drought in the Sahel. GeoJournal, 48, 299311.
Chander, G., Markham, B. L., & Helder, D. L. (2009). Summary of current radiometric calibration coefficients for Landsat MSS, TM, ETM+, and EO-1 ALI sensors. Remote Sensing of Environment, 113, 893–903.
Czajkowski, K., Goward, S., Mulhern, T., Goetz, S., Waltz, A., Shirey, D., & Dubayah, R. (2004). Estimating environmental variables using thermal remote sensing. In Thermal remote sensing in land surface processes. CRC Press.
Ji, L., & Peters, A. J. (2003). Assessing vegetation response to drought in the northern Great Plains using vegetation and drought indices. Remote Sensing of Environment, 87, 85–98.
Kogan, F. N. (1995). Application of vegetation index and brightness temperature for drought detection. Advances in Space Research, 15(11), 91–100.
Lo, C. P., Quattrochi, D. A., & Luvall, J. C. (1997). Application of high resolution thermal infrared remote sensing and GIS to assess the urban heat island effect. International Journal of Remote Sensing, 18, 287–303.
McKee, T. B., Doesken, N. J., & and Kleist, J. (1993). The relationship of drought frequency and duration of time scales. In Eighth Conference on Applied Climatology, Anaheim, CA, Jan 17–23, 1993 (pp. 179–186). American Meteorological Society.
Mishra, A. K., & Singh, V. P. (2010). A review of drought concepts. Journal of Hydrology, 203–212.
Mishra, A. K., Ines, A. V., Das, N. N., Khedun, C. P., Singh, V. P., Sivakumar, B., & Hansen, J. W. (2015). Anatomy of a local-scale drought: Application of assimilated remote sensing products, crop model, and statistical methods to an agricultural drought study. Journal of Hydrology.
Rizqi, I. S., Trisasongkoa, B. H., Shiddiqa, D., Imana, L. O., Kusdaryantoa, S., Manijoa, D., & Panuju, R. (2015). Identification of agricultural drought extent based on vegetation health indices of Landsat data: Case of Subang and Karawang, Indocase of Subang and Karawang, Indonesia. (T. 2.-I. Environmental, Ed.) Procedia Environmental Sciences, Elsevier.
Steininger, M. K. (1996). Tropical secondary forest regrowth in the Amazon: Age, area and change estimation with Thematic Mapper data. International Journal of Remote Sensing, 17, 09–27.
Tran, H. T., Campbell, J. B., Tran, T. D., & Tran, H. T. (2017). Monitoring drought vulnerability using multispectral indices observed from sequential remote sensing (Case Study: Tuy Phong, Binh Thuan, Vietnam). GIScience & Remote Sensing, 54(2), 167–184.
Tucker, C. J. (1979). Red and photographic infrared linear combinations for monitoring vegetation. Remote Sensing of Environment, 8(2), 127–150.
UNISDR. (2009). Drought risk reduction framework and practices: Contributing to the implemetation of the hyogo framework for action, Geneva, Swizerland. United Nations secretariat of the International Strategy for Disaster Reduction (UNISDR).
Vaani, N., & Porchelvan, P. (2017). GIS based agricultural drought assessment for the state of Tamilnadu, India using vegetation condition index (VCI). International Journal of Civil Engineering and Technology (IJCIET), 8(5), 1185.
Wang, H., Lin, H., & Liu, D. (2014). Remotely sensed drought index and its responses to meteorological drought in Southwest China. Remote Sensing Letters, 5(5), 413–422.
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Alam, A., Patra, P., Ghosh, A., Satpati, L. (2023). Identification of Spatio-Temporal Extent of Agricultural Drought Using Geospatial Techniques: A Case Study of Chhatna Block, Bankura District, West Bengal, India. In: Alam, A., Rukhsana (eds) Climate Change, Agriculture and Society. Springer, Cham. https://doi.org/10.1007/978-3-031-28251-5_6
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