Lesson 2 - Properties of Water Flashcards
What are some charateristics of water
- very strong
- Asymmetric
What happens to water when it freezes
Increase in volume
decrease in density –> expansion of water molecule at freezing allows ice to flow
Water molecules in gas phase
Highly charged with engergy
–> high energy state reduces likelihood of bonds between indiviual molecules
Two fundamental approaches to quantifying hydrology of landscapes:
General Water Balance Equation:
Quantitative (arithmetic) expression of the hydrologic cycle
Inputs – Outputs = Change in Storage
I - O = ∆S
Where:
I = Area inflows
O = Area outflows
∆S = Area Storage
Precipitation is defined as
The addition of fresh water to the earth’s surface from atmospheric water vapour in the
form of rain, snow, frost, fog, dew, etc.
Rain and Snow are the primary forms of precipitation
In the Okanagan Basin 80 to 90% of precipitation enters the basin as snow
Evapotranspiration Phase (ET) is defined as:
The total loss due to evaporation, interception and transpiration.
ET = E +It + T
In rough terms, about 60% of the total rainfall never reaches the soil due to Evaporation and transpiration in forested or grassland areas.
Evaporation (E) is defined as:
The transfer of water from the ground surface and from surface waters to the atmosphere resulting from solar radiation, temperature and wind velocity.
Interception total (It) is defined as:
The portion of rain that remains on above ground objects until its return to the atmosphere through evaporation.
Acts as temporary storage.
It = Ic + Ig
Transpiration (T) is defined as:
A biological evaporation process by which water within plants and vegetation, drawn through the root systems from the soil, is evaporated from the pores of leaves into the atmosphere.
Is dependent on weather conditions including temperature, wind, solar radiation, type of
vegetation
Is seasonal
Storage Phase (S)
Precipitation can be stored in a variety of ways including:
Surface waters
Snow and ice
Groundwater
Soil moisture
Depression storage
All of these types of storage are key components of the overall hydrological cycle.
Depression storage (Ds) refers to:
Precipitation which reaches the ground, is open to the atmosphere but does not immediately infiltrate or run off.
Lakes, rivers, ponds, puddles
Is described in terms of volume (m3, ft3, hectare metres, acre inches)
Runoff Phase (Q)
Runoff describes the amount of water from a watershed or drainage area resulting from precipitation, less evaporation and storage.
The end destination for all runoff is the oceans.
Components of Runoff:
Qtotal = Qsro + Qssro
Surface Runoff (Qsro) is described as
all flows over the earth’s surface