Dissolved Oxygen; Models; Reservoirs Flashcards
Dissolved CO2 in rivers varies
As a response to biological activity.
Models: can predict changes in (2)
Runoff, as a result of GH warming.
Streamflow, as a result of deforestation.
Residence time is an indication of
How quickly a water molecule in a reservoir can be renewed.
Residence time (years) =
mass in reservoir / flux into or from reservoir.
Dissolved oxygen: influenced by
Photosynthesis and respiration.
PS is limited at depth; O2 is reduced by respiration.
Dissolved oxygen: if levels fall below
Threshold, many organisms will die.
Dissolved oxygen: fall in oxygen levels may be
A result of sewage input.
Hydrological cycle: (2)
Driven by suns energy and gravity.
Evaporation exceeds precipitation over the oceans (vise versa).
Hydrological cycle: Exchange of water by (4)
Evaporation,
Infiltration,
Precipitation,
Surface run off to oceans.