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Precipitation in California primarily falls as rain or snow in the winter months, with significant variation across the state due to its diverse geography. Most of the precipitation occurs in the northern and mountainous regions, while the southern areas are drier. This uneven distribution leads to a reliance on reservoirs and the snowpack in the Sierra Nevada, which acts as a natural water storage system, releasing water gradually as it melts in spring and summer. Consequently, managing this variable water supply is crucial for agriculture, urban use, and ecological health in California.

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