joint gabls-glass/loco workshop, 19-21 september 2004, de bilt, netherlands interactions of the...
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![Page 1: Joint GABLS-GLASS/LoCo workshop, 19-21 September 2004, De Bilt, Netherlands Interactions of the land-surface with the atmospheric boundary layer: Single](https://reader036.vdocuments.mx/reader036/viewer/2022070307/551b7695550346a10a8b4c35/html5/thumbnails/1.jpg)
Joint GABLS-GLASS/LoCo workshop, 19-21 September 2004, De Bilt, Netherlands
Interactions of the land-surface with the atmospheric boundary layer:
Single column model experimentsat Cabauw, Netherlands
• evaluation of land-surface and ABL schemes at Cabauw, in offline and single-column (coupled) modes
• examine the role of soil moisture in boundary-layer evolution and cloud development (shallow cumulus)
Michael EkNCEP/EMC, Camp Springs, Maryland USA(work with Bert Holtslag, Wageningen Univ.)
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The interaction of the land-surface with the atmospheric boundary layer includes many processes and important feedback mechanisms.
land-surface/ABL interactions
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Coupled land-surface PBL model
• surface radiation simple incoming solar, longwave, albedo
• OSU land-surface multi-soil layers, simple canopy, Jarvis-Stewart conductance (Mahrt and Pan, 1984)
• ABL boundary-layer K-theory + nonlocal ABL mixing (Troen and Mahrt, 1986)
• surface layer M-O theory functions• ABL cloud cover turbulent + mesoscale RH dist’n
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Cabauw, Netherlands• central NL 45km east of N.Sea
• short grass, clay soils
• 213m tower obs
• micromet sitesurface fluxes, soil moisture & temp, radiation
• radiosondes: Cabauw & DeBilt
• 31 May 1978fair weather day
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- first represent soil-vegetation system in offline model runs using land-surface-only model- drive with observed atmospheric forcing- using existing formulations without tuning model parameters
land-surface-only interactions
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temperature
specific humidity
wind speed
incomingsolar
downwardlongwave
reflectedsolar
initial soiltemperature
initial soilmoisture
sensitivity testsdry moist
ATMOSPHERIC FORCING &INITIAL SOIL CONDITIONS
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latentheatflux
sensibleheat flux
canopyconductance
constant
reference
NP89
NP89 &PILPS2aroots
inferred obs
• Beljaars and Bosveld (1997) derived for Cabauw (reference)
CANOPY CONDUCTANCE TESTS• infer ‘observed’ canopy conductance from observations
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root densityprofiles
• PILPS2a root distribution yields underpredicted latent and overpredicted sensible heat fluxes due to soil moisture in upper soil layer depletion (higher root density) compared to reference case with a more uniform root density
reference
PILPS2a
uniform
soil moisture(4 model layers)
latent heat flux
sensible heat flux
ROOT DENSITY TESTS
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SOIL HEAT FLUX FORMULATION
vegetation effect:account for vegetation
cover with less soil heatflux throughvegetation
bare soil formulation:excessive soil heat flux
through vegetation
soilvegetation
reference
bare soil
latent heat flux
sensible heat flux
soil heat flux
• due to excess soil heat flux (bare soil case) model skin and soil temps lower compared to obs reference case
surface skintemperature
upper soillayer temperature
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SENSITIVITY TO INITIAL SOIL MOISTURE(LAND-ONLY MODEL RUNS)
• vary initial soil moisture +/- 5% (vol.) at surface, decreasing with depth
dry moist
• latent (sensible) heat flux increases (decreases) by about 28% (32%)• surface temperature decreases net radiation increases by <5%• reduced near-soil-surface temperature gradient soil heat flux decreases by 28%
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ABL-only interactions
- follow with ABL-only model runs (driven by observed surface fluxes)- then coupled column model runs, with prescribed (observed radiation) and modelled radiation (more fully interactive)
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INITIAL ABL CONDITIONS
• specify winds focus on ABL thermodynamics
• initial profiles of potential temperature and specific humidity
potentialtemperature
specifichumidity
saturationspecific
humidity
• profiles of wind speed(and Cabauw tower time series)
windspeed
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SENSITIVITY TO PRESCRIBED VERTICAL MOTION
• a nominally small vertical motion value yields ABL cloud fractions consistent with 31 May 1978 obs
Cloud cover and maximum afternoon ABL depth as a function of prescribed
vertical motion
• Cloud cover increases with increasing prescribed large-scale vertical motion (ABL-only model runs)
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ABL DEPTH & CLOUDS
• ABL growth slightly too vigorous in morning, better predicted in afternoon, transition to shallow SBL
• afternoon cloud fractions qualitatively consistent with obs in central NL
• results similar for ABL-only, and coupled land-ABL model runs
ABL depth
afternoon ABLcloud cover
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POTENTIAL TEMP & SPECIFIC HUMIDITY:TIME SERIES AND 12 UT PROFILIES
20-m potentialtemperature
20-m specifichumidity
12UT potentialtemperature
proflie
12UT specifichumiidty
proflie
• results similar for ABL-only, and coupled land-surface-ABL model runs.
• potential temp: slightly warmer in morning, cooler in afternoon
• specific humidity: less mid-morning ‘peak’ prior to late-morning rapid ABL growth, and more well-mixed.
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SURFACE FLUXES &RADIATION
• surface fluxes in coupled model runs compare well with offline land-only model runs, and observations.
latent heat flux
sensible heat flux
soil heat flux
net radiation
• radiation terms well-represented using our simple surface radiation formulation.
incomingsolar
downwardlongwave
reflectedsolar
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SUMMARY: LAND-SFC/ABL MODEL RUNS
• Model parameterization updates include modifications to land-surface formulations……canopy conductance at Cabauw (Beljaars and Bosveld 1997)
…soil heat flux formulation (account for vegetation cover) …plant root density (nearly uniform) …and a change to the boundary-layer depth formulation.
• For land-surface-only, ABL-only, and when coupled in land-surface-ABL column model runs… …realistic daytime surface fluxes and atmospheric profiles and ABL clouds are produced.…results compare well with observations using un-tuned parameterizations.
• Processes are well-represented by our column model in this coupled land-atmosphere system.
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SENSITIVITY TO INITIALSOIL MOISTURE
IN COUPLED COLUMNMODEL RUNS
• as initial soil moisture decreased from observed values, ABL cloud cover 0
cloud cover
ABL depth
• initial conditions same as in previous coupled model runs, but now vary initial soil moisture from dry to moist
• soil moisture increased, ABL cloud cover decreases slightly. WHY? …many land-ABL interactions
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land-surface/ABL interactions:effect of soil moisture
DRY SOILno clouds
MOIST SOILsome clouds
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…INCREASEDABOVE-ABL STABILITY
• vary initial soil moisture: dry to moist, and INCREASE above-ABL stability…
surface fluxes similar to reference case ABL depth decreased ABL cloud cover increases with increasing soil moisture
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…DECREASEDABOVE-ABL STABILITY
• vary initial soil moisture: dry to moist, and DECREASE above-ABL stability…
surface fluxes similar to reference case ABL depth increased ABL cloud cover decreases with increasing soil moisture
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RH TENDENCY
surface evaporative fraction RH/t =(Rn-G)/(Lvhqs)[ef+ne(1-ef)] available energy term non-evaporative term
ne = direct effects of non-evaporative processes on RH tendency: ABL growth ne=Lv/cp(1+C)[q/h)+RH[(c2/)-c1)] dry-air entrainment ABL warming
Ek and Holtslag 2004
• ABL-top relative humidity (RH) expected to control cloud formation
• role of soil moisture involves complex surface-ABL interaction
• ABL-top RH tendency:
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“Normalized” relative humidity tendency, ef+ne(1-ef)
• ne<1 (surface moistening regime) RH tendency increases as ef increases, increasing probability of clouds with stronger above ABL stability or dry-air entrainment (limited)
• ne>1 (ABL-growth regime) RH tendency increases as ef decreases,high surface evap limits ABL growth and RH increase, so increasing probability of ABL clouds with low surface evap and weaker above-ABL stability
greatest RH tendency & ABL cloud potential: low surface evap & weak atmos stability (ne>>1)
Cabauw values/times
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CABAUW DATA ANALYSIS
• role of soil moisture increase ABL-top RH (ne<1) …except during mid-day rapid ABL growth when soil moisture modestly increases ABL-top relative humidity (ne<1)
• sensitivity tests
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STRONG STABILITY CASE
STRONG STABILITY, DRY SOIL, NO CLOUDS
• ne<1(surfacemoisteningregime)
STRONG STABILITY, MOIST SOIL, SOME CLOUDS
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WEAK STABILITY CASE
WEAK STABILITY, DRY SOILMORE CLOUDS
WEAK STABILITY, MOIST SOILLESS CLOUDS
• ne>>1ABL-growthregime
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• Findings above qualitatively consistent with Ek and Mahrt (1994) for HAPEX-MOBILHY data (summer 1986, SW France)
HAPEX-MOBILHY
• 13 June 1986, with strong atmospheric stability above the ABL and a larger observed evaporative fraction (ne<1)
…gave a similar mid-day ABL-top relative humidity as 22 June 1986, with weaker atmospheric stability and decreased soil moisture (ne>1)
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• change in above-ABL stability affects both dry-air entrainment and ABL growth (opposing processes in RH tendency)
• with drier above-ABL air, ne decreases
• if q > critical value (more dry, negative) …ne decreases with decreasing stability
• yields opposite results in our decreased stability test, so less clouds with decreasing soil moisture
BOUNDARY-LAYER GROWTHvs. DRY-AIR ENTRAINMENT
dry-air entrainment “wins” over boundary-layer growth
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FUTURE• examine data from other field programs, e.g. additional Cabauw, HAPEX-MOBILHY, CASES, SGP, BOREAS, etc.
• further land-ABL column tests to explore land-atmos interaction, RH tendency and clouds; large-scale model output
• near-surface RH tendency could be used to infer soil moisture given other terms in the RH tendency equation
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LS-ABL
interactions/references
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Boundary-layer clouds