Historical exposure to drought — Cropland soil moisture anomaly in Shiga

Shiga: Historical exposure to drought — Cropland soil moisture anomaly was -5.61 Percentage change in 2025. ◆ Volatile

Latest (2025)
-5.61 Percentage change
Change on year
down 319.9%
Rank
2230th
of 2975 regions
All-time high
4.55 Percentage change
in 1991
All-time low
-5.79 Percentage change
in 1986
Years of data
76
1950–2025

Historical exposure to drought — Cropland soil moisture anomaly in Shiga, 1950–2025

-5-2.502.55195019872025

Source: Organisation for Economic Co-operation and Development. Measured in Percentage change.

Analysis

In 2025, historical exposure to drought — cropland soil moisture anomaly in Shiga stood at -5.61 Percentage change.

Compared with earlier readings it is down 319.9% on the previous year and down 87.4% over ten years.

Over the whole period, historical exposure to drought — cropland soil moisture anomaly in Shiga peaked at 4.55 Percentage change in 1991 and was at its lowest, -5.79 Percentage change, in 1986.

Shiga ranks 2230th of 2975 regions on this measure, in the middle of the range.

The series is highly variable year to year, so single readings are best treated with caution.

Averages by decade

DecadeAverage LowestHighest Years
1950s 1.43 Percentage change -2.57 Percentage change 2.84 Percentage change 10
1960s 0.7013 Percentage change -3.34 Percentage change 2.94 Percentage change 10
1970s 1.7 Percentage change -0.1936 Percentage change 3.38 Percentage change 10
1980s -0.3842 Percentage change -5.79 Percentage change 4.2 Percentage change 10
1990s -0.1794 Percentage change -3.75 Percentage change 4.55 Percentage change 10
2000s 0.9692 Percentage change -2.65 Percentage change 2.94 Percentage change 10
2010s -0.0776 Percentage change -2.99 Percentage change 1.92 Percentage change 10
2020s -1.05 Percentage change -5.61 Percentage change 2.55 Percentage change 6

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Frequently asked questions

What is historical exposure to drought — cropland soil moisture anomaly in Shiga?
Historical exposure to drought — cropland soil moisture anomaly in Shiga was -5.61 Percentage change in 2025, according to Organisation for Economic Co-operation and Development.
What is the highest historical exposure to drought — cropland soil moisture anomaly recorded in Shiga?
The highest recorded value was 4.55 Percentage change in 1991.
What is the lowest historical exposure to drought — cropland soil moisture anomaly recorded in Shiga?
The lowest recorded value was -5.79 Percentage change in 1986.
How does Shiga rank for historical exposure to drought — cropland soil moisture anomaly?
Shiga ranks 2230th out of 2975 regions with data for 2025.
Is historical exposure to drought — cropland soil moisture anomaly rising or falling in Shiga?
Over the last ten years it is down 87.4%. The long-run trend across the full record is volatile.
Where does this Shiga data come from?
The figures come from Organisation for Economic Co-operation and Development, published as part of Historical exposure to drought — Cropland soil moisture anomaly. Statizoid updates them automatically from the source API.

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CSV · JSON — 76 observations, free to reuse under OECD Terms and Conditions (attribution required).

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Historical exposure to drought — Cropland soil moisture anomaly in Shiga. Statizoid, drawing on Organisation for Economic Co-operation and Development. Retrieved 20 August 2026, from https://environment.statizoid.com/stat/historical-exposure-to-drought-cropland-soil-moisture-anomaly/shiga/

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About this data

Indicator
Historical exposure to drought — Cropland soil moisture anomaly
Unit
Percentage change
Source
Organisation for Economic Co-operation and Development
Licence
OECD Terms and Conditions (attribution required)
Coverage
3,200 places, 243,200 data points, 1950–2025
Last refreshed

The dataset provides annual anomalies in land and cropland soil moisture content of the top soil layer (0 to 7 cm) compared to the reference period 1981-2010. Exposure indicators to drought have been prepared by the Organisation for Economic Co-operation and Development (OECD). Please see the working paper for a more complete description of the methods. The datasets span the period 1981-2024 and is the result of the use of a variety of geospatial data sources, including the ERA5-Land averaged monthly data of volumetric soil moisture and ESA CCI land cover data. Average anomalies have been calculated for both land and cropland exposure to drought. The dataset has a global coverage on a national level; on the sub-national TL2 level (i.e. large subnational regions) results are reported for all OECD countries as well as for Argentina, Brazil, China, India, Indonesia and South Africa. A number of aggregates are included: Euro area, European Union, Advanced economies, Emerging market economies, G7, G20, OECD, OECD Europe, OECD Asia Oceania, OECD Americas and the LAC region. Data source(s): Copernicus Climate Change Initiative land cover data and Copernicus Climate Data Store monthly soil moisture data based on the ERA5-Land reanalysis dataset. Contact: ENV.Stat@oecd.org