创建一个干旱指标使用降水数据?- 江南体育网页版- - - - -地球科学堆江南电子竞技平台栈交换 最近30从www.hoelymoley.com 2023 - 04 - 14 - t22:32:31z //www.hoelymoley.com/feeds/question/18932 https://creativecommons.org/licenses/by-sa/4.0/rdf //www.hoelymoley.com/q/18932 2 创建一个干旱指标使用降水数据? 贾里德 //www.hoelymoley.com/users/18665 2020 - 01 - 10 - t15:05:58z 2020 - 01 - 17 t15:12:46z < p >我现在工作在一个项目中,我需要创建一个指标来量化干旱。宾夕法尼亚州,我每天都会从许多NOAA降水降水数据指标(英寸/天)。我试图创建一个可以量化的指标降雨某些领域得到了多少,希望沸腾的一个数字。度量的目标是描述1960年的干旱。做这个最好的方法是什么?< / p >

I've looked into many scientific papers for similar metrics, but most use more in depth models, and not just daily precip data. What are some good ideas? Average daily/weekly/monthly? Average number of days without rainfall?

//www.hoelymoley.com/questions/18932/-/18992 # 18992 2 回答为创建干旱指标使用Nemesi降水数据? Nemesi //www.hoelymoley.com/users/8087 2020 - 01 - 17 t15:12:46z 2020 - 01 - 17 t15:12:46z < p >的一个最广泛使用的指数来量化干旱事件标准化降水指数(SPI),它实际上是基于降水时间序列。使用索引等,也由< a href = " https://www.cpc.ncep.noaa.gov/products/Drought/Monitoring/spi.shtml " rel = " nofollow noreferrer " > NOAA < / >。< / p >

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I'll borrow the description of the index from a scientific article (Farinosi et al 2018)

Standardized precipitation Index (McKee et al., 1993)

The index is a measure expressed in standard deviation units of the variation of the precipitation of a specific number of months respect to the long run average (WMO, 2012). The number of months based on which the SPI could be calculated usually varies between 3 and 48 months. Shorter time scales SPI is considered a good indicator of variations of soil moisture, while on longer scales (up to 24 months), it could be associated with groundwater or reservoir levels variation (WMO, 2012). That for, a shorter SPI (3 months) is often utilized to detect meteorological droughts; a medium SPI (6 months) is usually associated with agricultural droughts; a longer SPI (12–24 months) is associated with hydrological droughts. SPI was calculated using the R package SPEI (Beguería and Vicente-Serrano, 2014).

Usually the minimum requirements to have a robust estimation of the SPI is to have a precipitation time series of at least 30 years.

You could use the SPI to quantify the number of "droughts" (choosing a threshold under which you define the event - for instance see this) in a period for your area of interest and then aggregate the number of "meteorological", "agricultural", and "hydrological" droughts.

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