Lecture12011.ppt
- 1. CE 374K Hydrology β Lecture 1 β’ Syllabus, sequence of topics β’ Hydrology as a science and as a profession β’ Hydrologic cycle and world water balance β’ Water as a physical substance β’ Water data sharing (separate Powerpoint presentation) Readings: β’ For today β Applied Hydrology and Chapter 1 β’ For Thursday, Applied Hydrology, Sections 2.1 and 2.2
- 2. Hydrology as a Science β’ βHydrology is the science that treats the waters of the earth, their occurrence, circulation and distribution, their chemical and physical properties, and their reaction with their environment, including their relation to living things. The domain of hydrology embraces the full life history of water on the earthβ From βOpportunities in Hydrologic Scienceβ, National Academies Press, 1992 http://www.nap.edu/catalog.php?record_id=1543 The βBlue Bookβ Has this definition evolved in recent years? Are new issues important?
- 3. Hydrology as a Profession β’ A profession is a βcalling requiring specialized knowledge, which has as its prime purpose the rendering of a public serviceβ β’ What hydrologists do: β Water use β water withdrawal and instream uses β Water Control β flood and drought mitigation β Pollution Control β point and nonpoint sources Have these functions changed in recent years? Are priorities different now?
- 5. Global water balance (volumetric) Land (148.7 km2) (29% of earth area) Ocean (361.3 km2) (71% of earth area) Precipitation 100 Evaporation 61 Surface Outflow 38 Subsurface Outflow 1 Precipitation 385 Evaporation 424 Atmospheric moisture flow 39 Units are in volume per year relative to precipitation on land (119,000 km3/yr) which is 100 units What conclusions can we draw from these data?
- 6. Digital Atlas of the World Water Balance (Precipitation) http://www.crwr.utexas.edu/gis/gishyd98/atlas/world.htm#animations
- 7. Global water balance Land (148.7 km2) (29% of earth area) Ocean (361.3 km2) (71% of earth area) Precipitation 800 mm (31 in) Evaporation 480 mm (19 in) Outflow 320 mm (12 in) Precipitation 1270 mm (50 in) Evaporation 1400 mm (55 in) Atmospheric moisture flow 316 mm (12 in) What conclusions can we draw from these data? Applied Hydrology, Table 1.1.2, p.5 (Values relative to land area)
- 8. Global Water Resources 105,000 km3 or 0.0076% of total water
- 10. Residence Time Residence time: Average travel time for water to pass through a subsystem of the hydrologic cycle Tr = S/Q Storage/flow rate Residence time of global atmospheric moisture (Ex. 1.1.1) Volume (storage) of atmospheric water: 12,900 km3 Flow rate of moisture from the atmosphere as precipitation = 577,000 km3/yr Tr = 12,900/577,000 = 0.022 yr = 8.2 days One reason why weather cannot be forecast accurately more than a few days ahead!
- 11. Water Molecule β’ Electrons desired β βsβ shell β 2 β βpβ shell β 8 β Total β 10 β’ Electrons available: β Hydrogen H1 β 1 β Oxygen O16 β 8 β For H2O β 10 http://www.brooklyn.cuny.edu/bc/ahp/SDgraphics/PSgraphics/SD.PS.LG.Water.html
- 12. Polar Bonding β’ 10 β 50 times weaker than covalent bonds between atoms in a molecule β’ Water as a solvent -- more substances dissolve in greater quantities in water than in any other liquid http://www1.lsbu.ac.uk/water/hbond.html
- 13. Water Density β’ Water as a solid (ice) is less dense than it is as a liquid β’ Maximum density is at 4Β°C http://www.chem1.com/acad/sci/aboutwater.html