User:Cagneiduncan/Surface water

Surface Water

An example of surface water is Lake Kinney.

Surface water is water located on top of the Earth's surface such as rivers, creeks, and wetlands. This may also be referred to as blue water. The vast majority is produced by precipitation and water runoff from nearby areas. As the climate warms in the spring, snowmelt runs off towards nearby streams and rivers contributing towards a large portion of our drinking water. Levels of surface water lessen as a result of evaporation as well as water moving into the ground becoming ground-water. Alongside being used for drinking water, surface water is also used for irrigation, wastewater treatment, livestock, industrial uses, hydropower, and recreation. r It is recorded by the Environmental Protection Agency (EPA), that approximately 68 percent of water provided to communities comes from surface water. For USGS water-use reports, surface water is considered freshwater when it contains less than 1,000 milligrams per liter (m/L) of dissolved solids.

There are three major types of surface water. Permanent (perennial) surface waters are present year round. This includes rivers, swamps, and lakes. Semi-permanent (ephemeral) surface water refers to bodies of water that are only present at certain times of the year including areas such as creeks, lagoons, and waterholes. Man made surface water is water that can be continued by infrastructure that humans have assembled. This would be lakes, dams, and artificial swamps. The surface water held by dams can be used for renewable energy in the form of hydropower. Hydropower is the forcing of surface water sourced from rivers and streams to produce energy.

Measuring Surface Water

A stream gage used to measure surface water.

Surface water can be measured as annual runoff. This includes the amount of rain and snowmelt drainage left after the uptake of nature, evaporation from land, and transpiration from vegetation. In areas such as California, the California Water Science Center records the flow of surface water and annual runoff by utilizing a network of approximately 500 stream gages collecting real time data from all across the state. This then contributes to the 8,000 stream gage stations that are overseen by the USGS national stream gage record. This in turn has provided to date records and documents of water data over the years. Management teams that oversee the distribution of water are then able to make decisions of adequate water supply to sectors. These include municipal, industrial, agricultural, renewable energy (hydropower), and storage in reservoirs.

Climate Change Impacts

Due to climate change, sea ice and glaciers are melting rising contributing to the rise in sea levels. As a result, salt water from the ocean is beginning to infiltrate our freshwater aquifers contaminating water used for urban and agricultural services. It is also affecting surrounding ecosystems as it places stress on the wildlife inhabiting those areas. It was recorded by the NOAA in the years 2012 to 2016, ice sheets in Greenland and the Antarctic reduced by 247 billion tons per year. This number will continue to increase as global warming persists.

Global warming has a direct connection with the hydrologic cycle. It has increased evaporation yet decreased precipitation, runoff, groundwater, and soil moisture. This has altered our surface water levels. Climate change also enhances the existing challenges we face in water quality. The quality of our surface water is based off the chemical inputs from the surrounding elements such as the air and the nearby landscape. When these elements are polluted due to human activity, it alters the chemistry of the water. If no progress is made in regards to this pollution of our drinking water will we have to develop more technology to purify it increasing expenses.