One of the Earth's subsystems that constitutes all the available water supply present on Earth, in all its forms
The hydrosphere exists in the other subsystems independently, it comprises at least 75% of the Earth's surface
Water budget
The finite amount of water on the Earth, slowly added by volcanic eruptions and meteors from space, that has lasted for billions of years
Residence time
The average length of time spent by a water molecule in a reservoir. Generally, water molecules in larger reservoirs have longer residence time
Reservoir types and water forms
Saltwater reservoir
Freshwater reservoir
Saltwater reservoir
Saltwater constitutes at least 97% of the total water supply on Earth. Because of its saltiness, it must be distilled and refined before it can be used for consumption
Ocean
A very large body of saltwater that surrounds the entire land
The total volume of the world's oceans is approximately 1.35 × 10^9 km^3
The Earth contains five (5)—or four (4), depending on the reference material—oceans
Salinity
The measure of a saltwater's saltiness. Ocean water has a varied salinity between 33 and 37 ppm (parts per million), mostly from sodium chloride (NaCl) existing as both sodium and chloride ions
Major ocean zones / saltwater profile
Surface layer/zone
Thermocline
Deep zone
Surface current/circulation
Movement of saltwater caused by surface air currents, depending on the hemisphere, on the surface zone, creating slow, broad drifts confined at depths of 50–100 m
Thermohaline/ deep currents circulation/current
Movement of water in the deep zone caused by the active processes within the zone caused by differences in density, which are controlled by both temperature and salinity
Freshwater reservoir
Most of the freshwater (a form of water that is not saline) on Earth are stored in glaciers and ice sheets in regions mostly inaccessible by man. The ones that are usable and potable are found on shallow surfaces and underground
Glacier
A permanent body of solidified water (i.e., ice) primarily composed of recrystallized snow compacted together. Glaciers form on land, and they are made up of fallen snow that gets compressed into ice over many centuries. They move slowly downward from the pull of gravity. Most of the world's glaciers exist in the polar regions, in areas like Greenland, the Canadian Arctic, and Antarctica
Ice sheet
Mass glacial ice covering more than 50,000 km^2 in total land area, commonly seen in Greenland and Antarctica. Ice sheets contain about 99% of the fresh water on Earth, and are sometimes called continental glaciers
Permafrost
Any part of the lithosphere and/or the pedosphere that has been frozen for more than two (2) years. Mostly found in polar regions, permafrost can be as deep as 150 m and has amassed storage of at least 300,000 km^3 worth of freshwater
Surface water
Streams
Rivers
Lakes
Reservoirs
Streams
A moving body of surface water flowing downslope from higher elevations toward sea level via clearly defined channels, carrying dissolved substances and sediments. Land areas that allow water to flow into streams are known as watersheds or drainage basins. Stream and river waters contribute to surface runoffs, aiding the transport of sediments and dissolved substances. A stream has an interaction with groundwater, depending on how the stream water flows
Rivers
Streams with considerably more volume of surface water flowing in well-defined channels. Rivers constitute at least 0.0006% of the global water supply (about 1.6% of the surface water supply), estimating at around 2,120 km^3 worth of freshwater
Lakes
Large inland bodies of water, either fresh or saline. Essentially flat on the water's surface, it is exposed to the atmosphere and formed in places with deep depressions (i.e., low areas) by water being supplied by inlet rivers and/or streams, overland flow, and/or groundwater. Lakes are the largest surface freshwater reservoirs, despite freshwater being the smallest water type on Earth
Wetlands
Land areas whose surfaces are covered primarily with water, whose biological life also adapted to its presence (i.e., water). Highly sensitive, any changes in the wetlands' waters drastically affect life in them
Wetland types
Marshes
Swamps
Estuaries
Groundwater
Freshwater found in the rock and soil layers deep within the soil's surface. As a freshwater source, it is the largest liquid freshwater source, as glaciers and ice sheets are the largest solid freshwater source on Earth. Groundwater sources can be seen as hollow caves located underground, or it can be encased in stone layers. Such rock layers with water are called aquifers
Humans have depended on water for years, and this is evident in the way early settlements were located: near coasts and riverbanks
Even today, humans still depend on water resources for food, water, transportation, religious, and recreational activities
Human activities affecting water quality
Population growth
Migration from rural settlements to urbanized areas
Demands for greater food security and higher living standards
Increased competition
Pollution from factories, cities, and farmlands
Other activities for water degradation
Sedimentation
Acid mine drainage
Improper waste disposal
Overexploitation of known water supplies
Responses to natural phenomenon
The RepublicAct No.8041of 1995 NationalWater Crisis Act addressed the Philippines' water problems through an integrated water management program and the development of new water resources and conservation of identified watersheds, among other provisions