Lecture 1: Fundamentals of water 2 Flashcards
FLUXES:
Precipitation
Includes rainfall, fog, snow, dew, sleet, rime… (measured in mm)
The most significant hydrological flux in many environments
Variable diurnally, seasonally, inter-annually and in the long term
Highly spatially variable
In most places precipitation is dominated by rainfall
Basic types: convective, orographic, frontal
FLUXES:
Precipitation- important characteristics
Seasonality – within the year
Variability → in inter-annual totals
Reliability → consistency in timing and duration
Amount → total volume (depth) of rainfall
Duration → how long the rainfall lasts
Frequency → how often it rains
Intensity → amount per unit time
Monitoring climate
Chiquito catchment, Costa Rica : distributed monitoring stations
Monitoring climate (instrumentally : at (or near) the ground)- San Gerardo cloud forest, Costa Rica : instrumental tower
Measuring rainfall
standard totalling gauge
tipping bucket (recording) raingauge
space borne radar- ground based rainfall radar
Pan tropical rainfall assessments
WORLDCLIM – 1km monthly measured rainfall compiled from 47,554 stations
interpolated using splines with altitude as a co-variable, complied by Hijmans et al (2005)*
b) TROPICLIM- 1km monthly near-surface rainfall based on 8 years of approx. bi-weekly Tropical Rainfall Monitoring Mission (TRMM) 2B31 rainfall rate data, processed by Mulligan (2006).
Costa rica
wind-driven rainfall highly variable in tropical mountains according to their eastern exposure
Evapo-transpiration
Upward flux from land back to atmosphere
Potential ET controlled by solar radiation, temperature and atmos humidity and wind speed
Actual ET controlled by availability of water (incl surface area)
Comprising: Free water evaporation Soil evaporation Canopy interception loss Transpiration through stomata
Varies with climate and land surface properties
Used by animals (and plants) for cooling
Loss through stomata in plants during photosynthesis → water productivity (kg/mm) fundamental to agriculture
Annual radiation load is highest in the tropics because.
… the same radiation is spread over a much smaller area
(Lambert’s Cosine Law). NOT because the land is further away – the
Solar energy has already travelled 92,900,000 miles (149,476,000
km) from the sun so an extra 4-6 000 km makes no difference).
This sets up a latitudinal gradient in energy that drives the hydrosphere
measuring evapotranspiration
evaporation pan (PET)
lysimeter
eddy covariance systems
scintillometers
measuring transpiration
Leaf chambers
- thermal sap-flow
- sensors
Runoff
The lateral flux of water balance (precipitation minus actual evapotranspiration)
Depends on rate of rainfall vs rate of infiltration (hydro-crossroads)
Overland flow on land
Streamflow/runoff in rivers
Responsible for global river network
Connects landscapes upstream-downstream
Through flow
Slow flow through matrix
Faster flow through macropores
Important for redistribution in time and space
Ensures rivers are perennial