Hydrologie II, part II
zweiter teil
zweiter teil
Kartei Details
Karten | 96 |
---|---|
Sprache | English |
Kategorie | Geographie |
Stufe | Grundschule |
Erstellt / Aktualisiert | 29.12.2013 / 16.01.2017 |
Weblink |
https://card2brain.ch/box/hydrologie_ii_part_ii
|
Einbinden |
<iframe src="https://card2brain.ch/box/hydrologie_ii_part_ii/embed" width="780" height="150" scrolling="no" frameborder="0"></iframe>
|
Lernkarteien erstellen oder kopieren
Mit einem Upgrade kannst du unlimitiert Lernkarteien erstellen oder kopieren und viele Zusatzfunktionen mehr nutzen.
Melde dich an, um alle Karten zu sehen.
2 reasons for preferential flow paths
macropores: due to biological activity, roots, animals. usually close to the surface
fingering flows: unstable wetting fronts due to persistent flow patterns created by soil heterogenity
where does subsurface flow occure?
i) close to surface, between organic and mineral soil
ii) deeper, at interface between bedrock and soil
whats the equivalent infiltration capacity model?
assumes infiltration excess runoff
for long-term events and large catchments
R = P-K^
whats the bucket model?
based on saturation excess runoff
for relatively wet catchments and topographic controlled streamflows
Smax = Zsoil*(θsat-θr)
whats the equivalent inflitration capacity + initial abstraction method?
its a combination of equivalent infiltration cap and bucket model.
first saturation excess is used (bucket), then infiltration excess
R = (P-Ia)-K^
what is the φ method?
a percentage of rainfall is used to generate runoff
for short events and small catchment areas,used for design small hydraulic structures
R=φ*P
3 conceptual models based on saturation excess mechanism
topmodel
vic model
pdm model
how does the topmodel work?
overland flow occurs when the water table crosses the topographic surface thus determining a saturated area which contributes to the overland flow. its a topographically controlled model.
when is the topmodel used?
when topography is very distinctive or no data is available (except a DEM)
hypothesis of topmodel
there is a saturated zone in equilibrium with a steady state recharge rate over an upslope contributing area "a". qi = P*ai
water table is parallel to the surface auch that the effective hydraulic gradiant is equal to the slope of the local surface qo=T(zi)*tan(ßi)
only gravity, no capillarity
stationary conditions qo=qi
hydraulic conductivity decreases exp with depth
depth of bedrock Z is much larger than depth of water table zi
physical mechanisms of rainfall runoff processes
non linear
time varying
distributed in space
characterized by heterogenities, anisotropies....
"randomly" varying in time and space
assumptions rainfall runoff transformations
linearity: I1(t)*e -> o1(t)*e, I1+I2->o1+o2
time invariance: I1(t)->o1,I2(t+tau)->o2
lumped description
-> linear model, conceptual and lumped describtion of basin response
what is evaporation influenced by?
topography, land use, meteorology, water availability..
what is the most important component of the water balance?
evapotranspiration
evaporation impacts..
water availability, hydrograph shape and peaks
solar constant
solar declination
I0=1366 W/m2
delta= 23.45°
equation of radiation
Ri = Rr + Ra + Rt
incoming = reflection + absorbtion + transmission
what causes diffuse radiation?
scattering of incoming radiation
Rsw = Rdir + Rdif
Radiation at the top of the atmosphere?
and on the surface?
Rsw = I0/4 = 342 W/m2 (due to shape and night)
surface = 188 W/m2
kirchhoffs law
R1/a1=R2/a2 or R1/e1=R2/e2
a: absorptivity, e: emissivity
"a good reflector is a bad emitter"
a=1 -> black body
plancks law
R= R(lambda, T),
Rtot = integral from 0 to infinity over R(lambda)d_lambda
wiens law
lambda_max = b/T
b: wiens konstant = 2898 um/K
describs the displacement of the wavelength with max radiation depending on the Temperature
stefan bolzmann law
Rtot = sigma * T4
radiation as a function of Temperature
albedo
alpha = Rr/Ri
alpha = alpha(lambda)
net radiation
Rn = Rsw(1-alpha) + RLW_in - R_LW_out
Rn = reflected + atmos - surface
RLW_in = ecs*K*sigma*TA4
RLW_out = es*K*sigma*Ts4
K is funct of cloud cover
e is frunct of vapour presure and temp
energy balance
Rn - lambda*E - H - G -Lp*Fp + AH = dU/dt
net radiation - latent heat - sensible heat - ground heat flux - energy from carbon fluxes (photosynthesis) + energy advection = energy stored in the system
simplified energy balance
Rn - lambda*E -H -G =0
-
- 1 / 96
-