Hydrologic cycle
Residence time= average length of time that water spends in a reservoir=reservoir size/yearly flux
Average residence times:
-oceans= 4,000 years
-glaciers= 20-1,000 years
-seasonal snow cover=2-6
-soil moisture=1-12 months
-groundwater 100 to 10,000
-lakes 50-100 years
-rivers 2-6 months
-atmosphere 10 days
Rainfall patterns
Controlled by large-scale atmospheric circulation
Atmospheric circulation
Low pressure at the surface where air rises- moisture condenses as air rises and cools and rainfall occurs
High pressure where air sinks-air is dry and deserts form
Monsoon
Seasonal sea breeze significant for precipitation
El Nino/La nina
Interannual changes in ocean and atmospheric circulation across the tropical pacific
Impacts rainfall patterns
Current el nino/la nina conditions
Current la nina conditions returning to enso-neutral
Climate change and precipitation
Increases and drought event
Drought
Deficiency of precipitation over a prolonged period of time, usually at least one season
Reduced surface and groundwater levels
Ca experienced a 3 year record drought 2013-2015
Flooding in california
Major floods in winter 2023-2024 ca has a history of major floods but exacerbated by climate change
Groundwater
Water present in the subsurface including soil moisture as well as water below the water table
-water table= upper surface in the earths below which all pore spaces in sediments and rocks are filled with water
Water can exist in aquifers= rock and sediment units below the surface that can hold and transport water
Aquifers in california
During an average year, 515 groundwater basins contribute about 38% of the states total water supply, but this increases to about 46% in drought years
Overdraft
If supply of water to a water-table aquifer is less than its discharge, the water table will lower, decreasing the size of the aquifer
Rives
Two sources: runoff and baseflow (water below the water table)
Drainage basin is the land surface from which all the surface runoff drains: also called a watershed
Glaciers
Glaciers are large accumulations of ice that exist year-round on the land surface
Supply many rivers (Himalayan glaciers, “The third Pole” supply brahmaputra, ganges, indus , mekong, and yangtze rivers
Climate change and melt water
Higher temperatures leading to greater summer melt
Smaller area of ice and snow cover means less melt water with time
Peal discharge is shifting to late spring/early summer
Climate change and sea level
Sea level rise is due to thermal expansion of seawater and melting of glaciers
Rising sea levels causing seawater invasion of coastal freshwater aquifers