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![Page 1: Min-Hui Lo, Wen-Ying Wu, Ren-Jie Wu Department of Atmospheric ...](https://reader033.fdocuments.in/reader033/viewer/2022052305/5890476f1a28abc1328c1e42/html5/thumbnails/1.jpg)
Applications of Remote Sensing Dataset on Studies of Biases in Land Surface Models (LSM)
Min-Hui Lo, Wen-Ying Wu, Ren-Jie Wu
Department of Atmospheric Sciences, NTU
2015/06/03 @ CWB
(1) Simulations of Land Water Storage in Australia(2) Simulations of Latent Heat Fluxes in California
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What is GRACE – global water cycle
Snow No Snow
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GRACE is like a giant scale in the sky that tells you how much weight you’ve gained or lost each month
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Implications for terrestrial and global hydrologyMass variations in Earth’s global water reservoirs
SGLOBAL = SOCEAN + SLAND + SICE = 0
We can now track ocean, land and ice changes using a single
observing system
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Global Water Storage
Courtesy of JT Reager
Total Oceans
Total Land
Total Oceans(seasonal cycle removed)
IPCC AR5
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Changes in Land water Storage
• A transition from El Nino to La Nina->more P on the land
• Persistence time of TWS over AUS is longer.
Extra Water
AUS
NA
SA
Australia includes expansive arheic and endorheic basins that impede runoff to ocean.(Fasullo et al.,2013)
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A unique endorheic (inland) river system in Australia
http://webworld.unesco.org/water/ihp/publications/waterway/webpc/pag13.html
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Can LSM simulate such changes?
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Models vs Observations
• GLDAS included results from three land models: NOAH, Mosaic , Vic, CLM2• Land Water Storage in GLDAS: canopy water, snow, soil moisture
Differences between models and
observations:
• Amplitude of Annual cycle
• Interannual varibility• Long term trend• Flood/Drought Event
(Flooding/decaying period)
Factor:• Interaction between
storage and transport• Water capacity
(Ground Water component, depth)
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Simulations in CLM4 with groundwater components
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Comparisons of GLDAS, CLM4, GRACE
However, there still are some discrepancies
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Short Summary I
• Global TWS is able to cause the temporary seal level variability; while the hydrologic process plays a crucial role.
• GRACE provided a new method to estimate the variability of TWS, which is available for examination the water storages simulated in land surface models.
• The component of groundwater should be into the land model with realistic mechanism.
• The mechanisms whereby water transport influences TWS might impact the climate?
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Simulations of Latent Heat Fluxes (Evapotranspiration) in California
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Irrigation intensity map (FAO)
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modified from Faunt et al., 2009
Water budget in heavily irrigated system
Central Valley Aquifer
Central Valley Surface Processes
GWR (184)
precipitation(374)
E(607)
surface water deliveries (241)
groundwaterwithdrawal
(203)storage lose (33)
(unit: mm/year)
California’s Central Valley(52,000 km2)
• Is one of the most productive agricultural regions in the world
• Produces 1/4 of the food in the U.S.
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1) CLM 2) MOSAIC3) NOAH4) VIC
How about the current LSMs?
Compare the ET of 4 different LSMs to observations
2003 2004 2005 2006 2007 2008 20090
100
200
300
400
500
Time
mm
/year
Average Preciptation over CV
Observational-based estimated ET from Anderson et al., 2012
from Anderson et al., 2015
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How to solve this ET discrepancy?
Representation of water withdrawals in the model
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dS
dt= In -Out
Inverse approach
Obs: 700 mm/yr
Model: 350 mm/yr
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GRACE ( from 2003~2010) dS
dt
60 mm/yr of decline
dS
dt= In -Out
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Surface water and groundwater withdrawals
160 mm/yr
190 mm/yr
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OBS
Results
from Anderson et al., 2015
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0 2 4 6 8 10 120
10
20
30
40
50
60
70
80
90
100
Month
Evap
otr
an
sp
ira
tion
, m
m/m
on
thClimatological Evapotranspiration, Averaged in Central Valley
obs
CMIP5
from Anderson et al., 2015
Simulations of Evapotranspiration in CMIP5
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Caveat:
• Constant irrigated water?
• GW withdrawal from confined and unconfined aquifers globally?
Future work:
• Apply this approach globally
• Couple to GCM to see human fingerprint on the climate
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Summary
• How to best utilize the GRACE data in climate model? at the seasonal forecast?
• Integrate GRACE information into the LSM
Thanks!
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ET estimates by MODIS
Using satellite data to quantify anthropogenic fluxes globally
Total water storage variationsfrom GRACE
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Total Water Storage Changes in the Combined Sacramento-San Joaquin River BasinsFrom the NASA GRACE Satellite Mission for March 2002- December 2013
Data courtesy of UC Irvine, National Center for Atmospheric Research, University of Texas, NASA
Courtesy of Jay Famiglietti
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Long-term
GRACEpereiod
(CLM4.0)
Precipitation