zong-liang yang the university of texas at austin
DESCRIPTION
Introduction to Land Surface Modeling. Zong-Liang Yang The University of Texas at Austin. Prepared for the TCEQ Meeting May 24, 2006 www.geo.utexas.edu/climate. Why Land Surface Modeling?. An important component of the weather, climate or environmental system. - PowerPoint PPT PresentationTRANSCRIPT
Zong-Liang Yang
The University of Texas at Austin
Introduction to Land Surface Introduction to Land Surface ModelingModeling
Prepared for the TCEQ MeetingMay 24, 2006
www.geo.utexas.edu/climate
Why Land Surface Modeling?
• An important component of the weather, climate or environmental system.– exchanges of momentum,
energy, water vapor, CO2, VOC, and other trace gases between land surface and the overlying atmosphere
– states of land surface (e.g., soil moisture, soil temperature, canopy temperature, snow water equivalent)
– characteristics of land surface (e.g., roughness, albedo, emissivity, soil texture, vegetation type, cover extent, leaf area index, and seasonality)
• Critical for weather, climate, hydrological, and environmental forecasts. NCAR CLM Website
The Development of Climate models, Past, Present and Future
Atmosphere Atmosphere Atmosphere Atmosphere Atmosphere Atmosphere
Land surfaceLand surfaceLand surfaceLand surfaceLand surface
Ocean & sea-ice Ocean & sea-ice Ocean & sea-ice Ocean & sea-ice
Sulphateaerosol
Sulphateaerosol
Sulphateaerosol
Non-sulphateaerosol
Non-sulphateaerosol
Carbon cycle Carbon cycle
Atmosphericchemistry
Ocean & sea-icemodel
Sulphurcycle model
Non-sulphateaerosols
Carboncycle model
Land carboncycle model
Ocean carboncycle model
Atmosphericchemistry
Atmosphericchemistry
Off-linemodeldevelopment
Strengthening coloursdenote improvementsin models
Mid 1950s Late 1960s Early 1980s Mid 1990s Present day Late 2000s?
John Houghton
Climate Change and Variability
P
E
Qs
Ss
Sg
Qg
Ig
Coupled Ocean-Atmosphere
Models
Hydrologic/Routing Models
Water Resources Applications
In Situ Data
Mesoscale Models
Air Quality Models
Soil-Vegetation-Atmosphere Transfer
Remote Sensing and GIS
Policy
Water Quality and Quantity
Air Quality
Integrated Environmental Modeling Framework
Tra
nsp
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Tra
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ran
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Fo
reca
st
Lea
d T
ime
Fo
reca
st
Lea
d T
ime
Warnings & Alert Warnings & Alert CoordinationCoordination
WatchesWatches
ForecastsForecasts
Threats Assessments
GuidanceGuidance
OutlookOutlookP
rote
ctio
n o
f P
rote
ctio
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f L
ife &
Pro
pe
rty
Life
& P
rop
ert
yP
rote
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f P
rote
ctio
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f L
ife &
Pro
pe
rty
Life
& P
rop
ert
y
Sp
ace
S
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ce
Op
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tion
Op
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tion
Sp
ace
S
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Op
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tion
Op
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tion
Re
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atio
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ecr
ea
tion
Re
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atio
nR
ecr
ea
tion
Eco
syst
em
Eco
syst
em
Eco
syst
em
Eco
syst
em
Sta
te/L
oca
l S
tate
/Lo
cal
Pla
nn
ing
Pla
nn
ing
Sta
te/L
oca
l S
tate
/Lo
cal
Pla
nn
ing
Pla
nn
ing
En
viro
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en
tE
nvi
ron
me
nt
En
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en
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me
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Flo
od
Miti
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F
loo
d M
itig
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& N
avi
ga
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& N
avi
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Flo
od
Miti
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F
loo
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itig
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& N
avi
ga
tion
& N
avi
ga
tion
Ag
ricu
lture
Ag
ricu
lture
Ag
ricu
lture
Ag
ricu
lture
Re
serv
oir
Re
serv
oir
Co
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ol
Co
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Re
serv
oir
Re
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Co
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Co
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En
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En
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Co
mm
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Co
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Benefits
Hyd
rop
ow
er
Hyd
rop
ow
er
Hyd
rop
ow
er
Hyd
rop
ow
er
Fire
We
ath
er
Fire
We
ath
er
Fire
We
ath
er
Fire
We
ath
er
He
alth
He
alth
He
alth
He
alth
Forecast Forecast UncertaintyUncertaintyForecast Forecast UncertaintyUncertainty
MinutesMinutes
HoursHours
DaysDays
1 Week1 Week
2 Week2 Week
MonthsMonths
SeasonsSeasons
YearsYears
Initial Conditions
Boundary Conditions
Accurate Land Surface Modeling Is Critical for Seamless Suite of Forecasts
Paul Houser
Land-Atmosphere Coupling Strength
Koster et al. (2004), Science
What Are Land Surface Processes
Land surface processes function as– lower boundary
condition in Atmospheric Models
• Atmospheric Boundary Layer Simulation
• Climate Simulation• Numerical Weather
Prediction• 4-D Data Assimilation
– upper boundary condition in Hydrological Models
• Water Resources Estimation• Crop Water Use• Runoff Simulation
– interface for coupled Atmospheric / Hydrological / Ecological Models
Land Surface Models (LSMs)• Computer code describing land surface processes (also
called LSSs, LSPs, SVATs)– FORTRAN, C, … ...– Tens to thousands of lines
• There are a huge number of LSMs (100+ examples in literature)– many are just “research models’’, local-scale oriented, with
specific process emphasis– up to ~100 canopy, ~100 soil, ~100 snow, even ~100
atmosphere layers!
• LSMs in GCMs and Hydrological Models are less diverse– one dimensional, with 1-2 canopy, 1-10 soil, 1-10 snow layers– three general classes
• “Bucket” Models (no vegetation canopy)• “Micrometeorological” Models (detailed soil/snow/canopy
processes) + Greening• “Intermediate” Models (some soil/snow/canopy features)
Four Basic RequirementsFrequently-sampled (hourly or sub-hourly) weather
“forcing data” to “drive” LSMs• precipitation (rate; coverage, large-scale/convective)• radiation (shortwave, longwave)• temperature• wind components (u, v)• specific humidity• surface pressure
Initialization of state variables• soil moisture (liquid, frozen)• deep soil temperature
Specification of surface characteristics• vegetation cover percent and composition (ET, BVOC…)• soil type (soil moisture & hydrology)• topography (hydrology)• albedo (solar radiation & energy balance)• roughness (turbulence & momentum exchange)• root depth (water holding capacity & hydrology)
Validation of simulations of state variables and fluxes• soil moisture• sensible/latent heat fluxes• skin temperature
Best Known Examples
– “Biosphere-Atmosphere Transfer Scheme (BATS)”
– “Simple Biosphere Model (SiB)”– Community Land Model (CLM)– Noah
Community Land Model
Hydrology
Drainage
Canopy Water
Evaporation
Interception
SnowMelt
Sublimation
ThroughfallStemflow
Infiltration Surface Runoff
Evaporation
Transpiration
Precipitation
Soil Water
Redistribution
Ocean Lake
Snow
Soil Water
Ground Water
River Flow
Surface Runoff
Direct Solar
Radiation
Absorbed SolarRadiation
Diff
use
Sol
ar
Rad
iatio
n
Long
wav
e R
adia
tion
Reflected Solar Radiation
Em
itted
Lon
g-w
ave
Rad
iatio
n
Sen
sibl
e H
eat
Flu
x
Late
nt H
eat
Flu
x
ua0
Momentum FluxWind Speed
Soil Heat Flux
Heat Transfer
Pho
tosy
nthe
sis
Biogeophysics
NCAR CLM Website
Community Land Model Dynamic Vegetation
Vegetation Dynamics
0
0.3
-10 25 60Temperature (C)
g C
O2g
-1s
-1
Root
HeterotrophicRespiration
Ecosystem Carbon Balance
Growth Respiration
g C
O2g
-1s
-1
0 1 2
Foliage Nitrogen (%)
0 15 30
Temperature (C)
g C
O2g
-1s
-1
0 500 1000
Ambient CO2 (ppm)
Photosynthesis
0 -1 -2
Foliage Water Potential (MPa)
g C
O2g
-1s
-1
0 1500 3000
Vapor Pressure Deficit (Pa)
46
20
0 500 1000
PPFD (molm-2s-1)
46
20
46
20
Sapwood
0
0.01
-10 25 60Temperature (C)
g C
O2g
-1s
-1Foliage
0
0.5
-10 25 60Temperature (C)
g C
O2g
-1s
-1
0 15 30Temperature
(C)
Re
lativ
e R
ate
1
8
Soil Water (% saturation)
Re
lativ
e R
ate
0 1000
1
AutotrophicRespiration
Litterfall
NutrientUptake
NCAR CLM Website
Noah
NCEP Noah Website
Research Issues
• Obtaining and applying relevant “pure biome” data to test or calibrate LSMs
• Dealing with spatial/temporal heterogeneity• area-average parameters or tiling of land covers?• defining space-time structure of atmospheric inputs
• Making best use of remote sensing data for initialization, specification and validation
• Improving key processes• Snow/Frozen soil• Runoff generation/routing• “Greening” of LSMs (carbon balance and
vegetation dynamics)• Urban
CLM Subgrid Structure
Gridcell
Glacier Wetland Lake
Landunits
Columns
PFTs
UrbanVegetated
Soil Type 1
Keith Oleson
CLM Subgrid Structure
Gridcell
Glacier Wetland Lake
Landunits
Columns/PFTs
Vegetated
PerviousShaded WallRoof Sunlit Wall Impervious
Urban
Canyon Floor
Industrial
Medium Density
Suburban
Keith Oleson
Climate Science Program at UT-Austin
NOAA, Understanding and Simulation of the Effects of Vegetation on North American Monsoon Precipitation.
NASA/NOAA, Parameterization of Snow Cover Fraction in Climate and Weather Prediction Models.
EPA, Impacts of Climate Change and Land Cover Change on Biogenic Volatile
Organic Compounds (BVOCs) Emissions in Texas.
DHS, Regional Scale Flood Modeling for the San Antonio River Basin, 3-yr Graduate Fellowship to Marla Knebl.
NSF, Including Aquifer into the Community Land Model, 3-yr Graduate
Fellowship to Lindsey Gulden. [Groundwater and Runoff]
NASA, Using MODIS Data to Characterize Climate Model Land Surface Processes and the Impacts of Land Use/Cover Change on Surface Hydrological Processes.
www.geo.utexas.edu/climate
Climate Change and Variability
P
E
Qs
Ss
Sg
Qg
Ig
Coupled Ocean-Atmosphere
Models
Hydrologic/Routing Models
Water Resources Applications
In Situ Data
Mesoscale Models
Air Quality Models
Soil-Vegetation-Atmosphere Transfer
Remote Sensing and GIS
Policy
Water Quality and Quantity
Air Quality
Integrated Environmental Modeling Framework
Coupling Land Surface with Other Processes
NCAR CLM Website