Earth Science – Oceanography, Geology, Astronomy, Meteorology Science – Physical Sci, Life Sci, Earth Sci Hydrosphere Meteorology is the study of the weather and forces and processes that cause it. In order to understand how the weather works, meteorologists must understand how energy, air, and water move between the hydrosphere, atmosphere and lithosphere. - the water cycle Meteorologists – good at math and physics, visual problem solvers, good at seeing patterns/solving puzzles; making connections, seeing relationships, what stuff has in common – understanding how stuff fits together. Scientists have given names to the living, solid, liquid, and gas parts of the earth. The four spheres of Earth Science are: sphere = round, ball shaped (1) Biosphere – living (biologist) (2) Lithosphere – rocky, ground, solid (geologist) (3) Hydrosphere - water, liquid (oceanographer) (4) Atmosphere – air, gas (meteorologist) Cryosphere – ice (glaciologist) The living part of the Earth is called the Biosphere. The term is used to refer to the whole earth. Ecologists, Environmentalists, and other types of Life Scientists study the Biosphere. tectonic plate 60-100 miles thick Hydrosphere - 2 The lithosphere is the solid part of the earth. It is made up of rocks, minerals, and soil. The ground you walk on is part of the lithosphere. Mountains are part of the lithosphere. The lithosphere extends under the ocean and makes up the continents. It includes the earth’s crust and the top part of the upper mantle. Various types of geologists study the lithosphere. Useable Freshwater: 1mi3 = a cube 10,000 gal by 10,000 gal by 10,000 gal The hydrosphere is the liquid part of earth that is near or around the surface. About 71% of the earth’s surface is covered by water. The amount of water on earth is immense, an estimated 326 million cubic miles. A cubic mile of water equals more than one trillion gallons. However, 99.7% of all water States Geological Survey on earth is unusable by humans. United (USGS); NOAA 0.3% = 0.003 times 326 = 0.978 x/326 = 0.3/100 Useable Freshwater: 326,000,000 mi3 times 0.3% = 0.978 or about 1,000,000 mi3 or about 1,000,000,000,000,000,000 gallons or about 1quintillion gallons = 1 trillion million gallons of usable freshwater We use 0.4 trillion gal per day in the US. How deep are the world’s oceans, deepest lakes and rivers? This picture shows the size of a sphere that would contain all of Earth's water in comparison to the size of the Earth. The blue sphere sitting on the United States, reaching from about Salt Lake City, Utah to Topeka, Kansas, has a diameter of about 860 miles (about 1,385 kilometers) , with a volume of about 332,500,000 cubic miles (1,386,000,000 cubic kilometers). The sphere includes all the water in the oceans, seas, ice caps, lakes and rivers as well as groundwater, atmospheric water, and even the water in you, your dog, and your tomato plant. http://ga.water.usgs.gov/edu/2010/gallery/global-water-volume.html Hydrosphere -3 Salt Water 97.2349% of all water on earth is salt water and is unusable by living organisms. round to 97% oceans = 97.2269% - round to 97% salt lakes (inland seas) = 0.008% Remember 97% to 3% Remember 85% of freshwater is unusable Fresh water = 2.7651% - round to 3% Only 15% of the Earth’s freshwater can be used by living things. ice sheets and glaciers = 2.14% - not usable by living organisms ground water = 0.61% fresh water lakes = 0.009% rivers and streams = 0.0001% soil moisture (above the aquifer) = 0.005% atmosphere = 0.001% Remember most of earth’s usable freshwater comes from the ground! These numbers are good approximations, but they change constantly because of the water cycle! Remember 97% toHydrosphere 3% and 99.7% to 0.3% -4 Humans use an enormous amount of water. Each person uses about 80-100 gallons per day. In the year 2005, the United States used about 410 billion gallons per day (410,000 Mgal/d) of fresh water with a population of 281,421,906 people. At this rate of use, the US would use up the entire world’s supply of useable fresh water in 6570.84 years. Current population = U.S. 316,937,528; World 7,119,758,440 Oct 24, 2013 10:55 UTC (-4) http://www.census.gov/ Water usage is broken down into eight major categories. The following is what water was used for in the Unites States in 2005: thermoelectric power (hydroelectric) = 49% -thermal pollution irrigation (farming) = 31% public supply = 11% - you, me, city water industry = 4% aquaculture (fish farms) = 2% domestic (self-supplied wells) 1% mining = 1% livestock = <1% Environmental Protection Agency (EPA) Health of an ecosystem? Pollution + Biodiversity How much stuff is in the water? water hardness? mercury and lead? Hydrosphere - 5 Water pollution contains minerals, chemicals, or organisms that can disrupt life processes and cause disease or death. The largest source of water pollution is sediment - loose clay, mud, or minerals that have been eroded. There are two types of pollution. Ocean water 35-38 Point Source – known source, small area parts per thousand Non Point Source – source unknown, large area Freshwater versus polluted water – defined and classified storm drain pipe? Classified by the amount of pollutants: freshwater = 0 – 1000 ppm [parts per million or 1000 mg/l (milligrams per liter)]; 0-499 = drinkable; 500-999 potable Polluted water = greater than1000 ppm Polluted water area with excessive plant growth, dead animals, and lots of bacteria RED TIDE – toxic algae bloom in the ocean Algae Blooms: definition and 4-5 steps (1) pollution, fertilizers/run off enters lake, streams, rivers (2) algae populations grows out of control because of the fertilizers. As the algae dies, the bacteria population grows out of control (3) the bacteria consume all the oxygen in the water (4) all the animals die because of the lack of oxygen N–P-K Acid rain is a type of both water and air pollution. Polluted water = greater than1000 ppm Pollutants such as sulfur dioxide (SO2) or nitrogen oxide (NOx) enter the air from a source such as a power plant or volcano. The wind blows the pollutions far from the source. The pollutant lowers the pH (raises the acidity) of the water in the air. Pure water has a pH of 7.0. Normal rain is slightly acidic because carbon dioxide dissolves into it, so it has a pH of about 5.5. As of the year 2000, the most acidic rain falling in the US has a pH of about 4.3 which is 3 ways thatharmful water quality to is plant and animal life. very measured Water Quality a measure of the suitability of water for a particular use based upon selected characteristics. chemical: pH, dissolved oxygen, nitrates, phosphates, salts, hardness, iron, carcinogens, solvents, sediments physical: temperature, electrical conductivity, turbidity/ suspended particulates (muddiness) biological: bacteria - fecal coliform, protozoa, pathogens Point Source Pollution: pollution enters from a small area; the specific location is known. Non Point Source Pollution: pollution enters from a large area; the exact source is unknown. Hydrosphere - 6 Physical Property Although the percentage of fresh water available on earth is small, the earth never runs out because water is a renewable resource. This means its actual amount is not limited and it can be easily replenished. This happens because water can readily change from one state of matter (solid, liquid, gas) to another at the temperatures and pressures that occur around Earth’s surface. Water is constantly moving between each of the four spheres of Earth Science. This unending circulation of earth’s water supply is called the water cycle or the hydrologic cycle. It has several main steps: water storage evaporation / transpiration Water is renewable because it can exist and condensation change from a solid to a liquid to a gas on or near precipitation the surface of the earth! recharge of water storage Hydrosphere - 7 Even though water is renewable, it must be conserved because: (1) there is a limited amount; humans can use it up due to pollution and (2) humans can also use it faster than nature can replenish it. ocean = largest water storage area solid or liquid water water storage Water storage supplies are stored in lakes, streams, oceans, and snow fields. Man-made water supplies are called reservoirs. ground water = largest useable freshwater storage area glaciers – largest freshwater storage area water towers? evaporation / transpiration Evaporation is the process where liquid water is and becomes a gas called water vapor. Usually the sun heats the water supply and vaporizes it at its surface. Transpiration is the process by which water is evaporated into the air through plants (leaf pores). The sun drives the water cycle! gas – heated rises Adding heat turns liquid water into a gas Lots of spaces between molecules Temperature: speed or motion of particles; everything has a temp! Heated water vapor rises into the air because it is lighter. Hot light things rise!!!! Cold Heavy things sink!!! condense gas rise – cool, contract FROZEN – SOLID NO SPACE BETWEEN MOLECULES evaporate add heat expand liquid – cool some space between Hydrosphere -molecules 8 condensation Condensation is the process of changing water vapor (gas) held in the air into a liquid by removing heat - cooling. Water drops on the outside of a cold glass are condensed water. Where does the water come from? condensation point = dew point = temperature that gas changes into a liquid How does dew form? The temperature at which water vapor changes from a gas to a liquid is called the dew point or saturation point. When the dew point is close (within 5°F) to the air temperature, rain is very likely. Dew forms when moist air (water vapor) near the earth’s surface cools. If the surface temperature falls below freezing, then the dew turns into frost. Dew point is determined by pressure – weight of the air It is the temperature at which liquid water or dew evaporates at the same rate at which it condenses. less weight (lower pressure) = easier to condense = lower dew point; HP = high dew point Humidity is moisture or water in the atmosphere. The amount of humidity is determined by temperature. Higher temperatures mean higher humidity. Lower temperatures mean lower humidity. Hydrosphere - 9 condensation Relative humidity is a measure of how much water air holds at a certain temperature compared to the total amount of moisture that it can hold. It is measured in percent. When air is totally dry, the relative humidity is 0. When air holds half the water that it is able, the relative humidity is 50%. When air is completely full of water the relative humidity is 100%. When air reaches the point of 100% humidity, the air is saturated and water vapor will change from a gas to a liquid and it will rain. Specific Humidity: measures the actual quantity of water vapor in a given mass of air. It is measured in g/kg (parts per thousand) or g/m3 (parts per million) [1g=1cc=1ml water, 1m3=1000L]. Fog/clouds are liquid, not a gas! Fog is a mass of tiny liquid droplets of water that have condensed around dust particles (cloud seeds). The droplets are too tiny to fall and are held in place by air currents. Fogs/clouds need: Why do you see your breath when it is cold? What are dirty clouds? Why are clouds dark? cloud seeding – artificial clouds contrails? condensed trail: cloud made by an airplane How do you see tornados if they are just wind? 3 types of fog – advection, Hydrosphere radiation, and upslope - 10 (1) water vapor - gas (2) cooling agent (3) something to stick to condensation Fog forms on the ground when a layer of air is cooled to its dew point by contact with the colder surface. Clouds are very similar to fogs only they form at much higher altitudes. They are formed when a layer of moist air is cooled by another layer of air. Clouds are not water vapor; they are liquid water droplets too tiny to fall to Earth as precipitation. CLOUD temperature drops with height above the ground dew point temp cool air cooled from air above FOG cooled from ground below warm air warm air water gas cool ground Precipitation Precipitation is water that falls to earth from clouds in the atmosphere. When water droplets cool and condense, they get larger to the point that gravity pulls them back to the earth. There are five kinds based on their size: hail snow rain sleet 1- largest drizzle 5- smallest Hydrosphere - 11 precipitation 1/1000th inch, 14 μm The size of water vapor droplets is very small. Drizzle droplets are much smaller than rain droplets, but are much larger than water vapor droplets. When water droplets freeze on their way to the earth, sleet, snow, and hail form. Sometimes strong updrafts blow the droplets back up into the clouds where they gain another layer of water which refreezes. This process is how hail is formed. The largest hailstone ever recovered in the United States (South Dakota), a seven-inch (17.8-centimeter) wide chunk of ice almost as large as a soccer ball. 2 pounds; July, 2010 Removing heat (cooling) turns water vapor back into a liquid. Liquid water sinks or falls to the ground because it is heavy. Cool heavy things sink!!!! What is the shape of a rain drop? Hydrosphere - 12 2 types: above ground - runoff below ground – filling the aquifer/ground water recharge of water storage The recharge of water storage happens after precipitation hits the ground. The water follows surface contour lines as it flows as runoff into lakes, rivers, and the ocean. Gravity is the energy source! Water runs downhill! Nile River? Much of the water that hits the ground does not runoff. It percolates or moves downward through the pores and spaces in the soil until it hits the - a place where the soil is saturated or completely filled with water. This zone of saturation is an underground water storage area called an . If it rains so much that the water table moves to the surface, there will be a flood. If it rains so hard and fast that most of the rain runs off above the ground and does not go into the ground, do some rivers/lakes run then flash flooding occurs. Why dry in the summer? What is a flood plain? an area where the water table is always near the surface The rate of movement of ground water depends on the porosity and permeability of the ground. Porosity is the amount of void space or opening in a rock or other earth material like a sand deposit. It is how much water a material can hold. Water table and drought? Hydrosphere - 13 recharge of water storage Porosity represents the storage capacity of the ground material. It is measured in percent of open space. The more tightly packed the grains are, the lower the porosity. If the sizes of the ground particles are both large and small, the smaller grains tend to fill the spaces between the larger grains, resulting in lower porosity. Teayes River Valley? Cedar Bog/Fen Permeability refers to how well water flows through a material. It is controlled by how large the pores are, and how well connected they are. Materials such as clay and shale may have a high porosity because of lots of microscopic openings, but they have low permeability because the openings are not connected. So, water cannot pass through. Materials such as clay and solid rock that block water are called confining units. Well yields? Champaign Co/Logan Co How close is the bedrock to the surface? West of Hw 68: 500 to 1000 gal/min; East of Hw 68? East of 68: 3-8 to 100 gal/min The water in the aquifer moves due to gravity and eventually recharges or refills wells, reservoirs, lakes, rivers, and the ocean. This is how we get our water! surface runoff river or pond effluent stream: fed by the water table http://ga.water.usgs.gov/edu/ear thgwaquifer.html http://ga.water.usgs.gov/edu/earthgwaquifer.html