Rain is the most common form of precipitation and occurs when water droplets in the atmosphere become too heavy to stay suspended and fall to the ground. Rainwater can be collected and stored for later use, or it can be allowed to infiltrate the ground and recharge aquifers.
Snow is frozen precipitation that occurs when water vapor in the atmosphere forms ice crystals. Snow can accumulate on the ground and form snowpacks, which can provide a significant amount of water when they melt. Snowmelt can be used to fill reservoirs, generate hydropower, and irrigate crops.
In addition to rain and snow, sleet and hail can also be important in water resources engineering. Sleet is a mixture of rain and snow that occurs when snowflakes partially melt as they fall through warmer air near the ground. Hail is frozen rain that occurs when raindrops are carried up into the atmosphere by strong updrafts and then freeze. Hailstones can be as small as a pea or as large as a golf ball. Sleet and hail can damage crops and infrastructure, and they can also pose a hazard to life and limb.
The amount and type of precipitation that falls in a particular area can vary significantly from year to year. This variability can make it difficult to manage water resources effectively. Water resources engineers use a variety of tools and techniques to predict and manage precipitation, including:
* Rainfall-runoff models: These models simulate the way that precipitation falls on land and flows over and into the ground.
* Snowmelt models: These models simulate the way that snow melts and releases water into rivers and lakes.
* Climate change models: These models predict how climate change is likely to affect precipitation patterns in the future.
Water resources engineers use these tools and techniques to help water managers make decisions about how to best use and conserve water resources.
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