Which one is in a
drought?
Definition
Drought is not determined by how little precipitation a region receives. It is defined by how much precipitation falls relative to what is historically expected. A rainforest receiving half its normal rainfall may be experiencing drought, while a desert receiving its typical amount of precipitation may not.
Scientists measure these deviations using the Standardized Precipitation Index (SPI), a score that compares observed precipitation to a region's long-term average.
Concept
Because drought is defined by precipitation deficit rather than heat, it can occur across many climate zones, including mountain ranges, temperate forests, grasslands, and Arctic regions.
An SPI value below −1 generally indicates drought conditions, regardless of whether the local climate is hot, temperate, or cold.
Step 1
An SPI of 0 means precipitation is equal to the long-term average for that region. There is no surplus or deficit. This value serves as the reference point for identifying wetter or drier conditions.
SPI = 0.0
Step 2
A positive SPI indicates that precipitation was above the historical average. An SPI of +1.0 represents moderately wet conditions, while +2.0 indicates unusually wet conditions that may increase flood risk.
SPI = 0.0
Step 3
An SPI between −0.5 and −0.9 indicates below-average precipitation. These values may signal emerging dry conditions, although they are not typically classified as drought.
SPI = 0.0
Step 4
An SPI between −1.0 and −1.5 indicates moderate drought. At this level, a region has received substantially less precipitation than expected, which can affect streamflow, vegetation, and water availability.
SPI = 0.0
Step 5
An SPI of −2.0 or below indicates extreme drought. These events are statistically rare and may be associated with severe water stress, ecosystem impacts, and longer recovery periods.
SPI = 0.0
Why this matters
When a hot desert experiences a dry spell, the local infrastructure is already built for it. But when a cold, temperate, or high-altitude region slips into a persistent precipitation deficit, communities become vulnerable to unexpected climate events. Hidden droughts strike the places least prepared for them.
Food security
Temperate grasslands and continental interiors like Central Asia or the US Midwest grow the majority of the world's grain. A seemingly mild 15% drop below historical precipitation averages is enough to trigger global food price spikes and export bans.
Energy
Many cold and mountainous regions rely on winter snowfall to drive hydroelectric power. When cold droughts hit, alpine reservoirs dry up. Countries transitioning to green energy are suddenly forced back to coal and gas just to keep the lights on.
Geopolitics
Because these droughts don't "look" like a natural disaster, political responses are slow. Water-sharing agreements signed decades ago based on historical baselines are collapsing, turning river basins into geopolitical flashpoints.
Adjust temperature and precipitation to compare climate profiles across countries.
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DROUGHT RISK
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