Caribbean Evaporative Demand Drought Index
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https://data.lib.vt.edu/articles/dataset/Caribbean_Evaporative_Demand_Drought_Index/21543108/1
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ERA5-Land derived pentad evaporative demand drought index (EDDI) for the Caribbean from 1981-2021. EDDI is calculated following Hobbins et al. 2016 and the underlying input data are acquired from ERA5-Land (Muñoz-Sabater 2021). This version of EDDI calculates hourly ASCE reference evapotranspiration for a short reference surface following Allen et al. 2005. Leap days have been removed. <br> This dataset was produced by first creating hourly reference evapotranspiration for a short reference crop for every grid point in the study domain following the equations laid out in Allen et al. 2005. <br> Allen, R. G., I. A. Walter, R. L. Elliott, T. A. Howell, D. Itenfisu, M. E. Jensen, and R. L. Snyder, eds., 2005: The ASCE Standardized Reference Evapotranspiration Equation. American Society of Civil Engineers. <br> EDDI was calculated using 5-day (e.g. pentad) accumulated reference ET following Hobbins et al. 2016. <br> Hobbins, M. T., Wood, A., McEvoy, D. J., Huntington, J. L., Morton, C., Anderson, M., & Hain, C. (2016). The Evaporative Demand Drought Index. Part I: Linking Drought Evolution to Variations in Evaporative Demand, <em>Journal of Hydrometeorology</em>, <em>17</em>(6), 1745-1761. https://journals.ametsoc.org/view/journals/hydr/17/6/jhm-d-15-0121_1.xml <br> For more information regarding the hourly ERA5-Land inputs to the reference ET equations, please see Munoz-Sabater et al. 2021. <br> J. Muñoz-Sabater, Dutra, E., Agustí-Panareda, A., Albergel, C., Arduini, G., Balsamo, G., Boussetta, S., Choulga, M., Harrigan, S., Hersbach, H., Martens, B., Miralles, D. G., Piles, M., Rodríguez-Fernández, N. J., Zsoter, E., Buontempo, C., and Thépaut, J.-N.: ERA5-Land: A state-of-the-art global reanalysis dataset for land applications, Earth Syst. Sci. Data,13, 4349–4383, 2021. https://doi.org/10.5194/essd-13-4349-2021. <br> <br>
提供机构:
University Libraries, Virginia Tech
创建时间:
2023-09-28



