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Data used: Not relevant; 
Data format: N/A;
Data access: N/A;

Concise description:
The SGI builds on the Standardized Precipitation Index (SPI) to account for differences in the form and characteristics of groundwater level and precipitation time series. The SGI is estimated using a non-parametric normal scores transform of groundwater level data for each calendar month. These monthly estimates are then merged to form a continuous index.</gco:CharacterString>
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  <Drought xmlns:delta="http://www.deltares.nl/delta">
    <GeneralCharacteristics>
      <Model_Name>Standardized Groundwater Index (SGI)</Model_Name>
      <Characteristics_Goals>This index can be used to determine and characterize groundwater drought hazards.</Characteristics_Goals>
      <type>Indices</type>
      <DroughtType>Hydrological</DroughtType>
      <Applications>Mapping hydrological drought hazard</Applications>
      <Status>N/A</Status>
      <!--Indices_Included>N/A</Indices_Included>
		<Countries_where_available>Not relevant</Countries_where_available>
		<Period_available_From>Not relevant</Period_available_From>
		<Period_available_To>Not relevant</Period_available_To>
		<Costs>None</Costs-->
      <Concise_description>The SGI builds on the Standardized Precipitation Index (SPI) to account for differences in the form and characteristics of groundwater level and precipitation time series. The SGI is estimated using a non-parametric normal scores transform of groundwater level data for each calendar month. These monthly estimates are then merged to form a continuous index.</Concise_description>
    </GeneralCharacteristics>
    <Contact_information>
      <Links>http://www.hydrol-earth-syst-sci.net/17/4769/2013/</Links>
      <Organization>N/A</Organization>
      <Contact_person>J.P. Bloomfield</Contact_person>
      <!--Contact_details>jpb@bgs.ac.uk</Contact_details-->
      <Resource>The following package requires Matlab and a MathWorks Account: https://nl.mathworks.com/matlabcentral/fileexchange/51081-standardized-drought-analysis-toolbox--sdat-</Resource>
    </Contact_information>
    <!--Data_and_links>
		  <Data_requirements>Groundwater levels</Data_requirements>
		  <Data_used>Not relevant</Data_used>
		  <Data_format>N/A</Data_format>
		  <Data_access>N/A</Data_access>
	  </Data_and_links-->
    <Spatial_and_temporal_scale>
      <!--Spatial_reference>Spatial_reference</Spatial_reference>
		<Spatial_Scale>Not relevant</Spatial_Scale>
		<Spatial_Extent>-180, 180, 90, -90</Spatial_Extent>
		<Temporal_Scale>Monthly</Temporal_Scale>
		<Aggregation_Period>Not relevant</Aggregation_Period-->
      <Latency>N/A</Latency>
    </Spatial_and_temporal_scale>
    <Quality_and_references>
      <References>Bloomfield, J. P. and Marchant, B. P.: Analysis of groundwater drought building on the standardised precipitation index approach, Hydrol. Earth Syst. Sci., 17, 4769-4787, https://doi.org/10.5194/hess-17-4769-2013, 2013. 

 Bloomfield, J. P., Marchant, B. P., Bricker, S. H., and Morgan, R. B.: Regional analysis of groundwater droughts using hydrograph classification, Hydrol. Earth Syst. Sci., 19, 4327-4344, https://doi.org/10.5194/hess-19-4327-2015, 2015.

Haas, J. C., and Birk, S. (2015, December). Identifying Groundwater Droughts using standardized Water Levels. In AGU Fall Meeting Abstracts.</References>
      <Strengths>N/A</Strengths>
      <Weaknesses>Weaknesses are largely similar to that of SPI: dependent on length of available timeseries,assumed distribution of groundwater levels. Additionally dependent on local recharge patterns. Low groundwater levels do not necessarily indicate serious drought. Additionally, the indicator has no real history of use.</Weaknesses>
      <Quality>N/A</Quality>
    </Quality_and_references>
  </Drought>
</gmd:MD_Metadata>

