1 Indirect evidence of vertical humidity transport during very stable conditions at Cabauw Stephan...

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1 Indirect evidence of vertical humidity transport during very stable conditions at Cabauw Stephan de Roode ([email protected] ) Clouds, Climate and Air Quality Department of Multi-Scale Physics (TNW) Stephan R. de Roode (TU Delft) & Fred C. Bosveld (KNMI)

Transcript of 1 Indirect evidence of vertical humidity transport during very stable conditions at Cabauw Stephan...

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Indirect evidence of vertical humidity transport during very stable conditions at Cabauw

Stephan de Roode ([email protected])Clouds, Climate and Air Quality Department of Multi-Scale Physics (TNW)

Stephan R. de Roode (TU Delft) &

Fred C. Bosveld (KNMI)

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Stable boundary layers -Analysis of Cabauw data for the period 2001-2006

selection criterion height data fraction

I. nighttime 1m 0.50

II. clear sky 1m 0.18

III. weak wind 10m 0.08

IV. stable 5m 0.07

V. surface cooling 2m 0.05

SWnet <1 Wm-2

LWnet > 40 Wm-2

U tot < 3 ms -1

RiB > 0

dT

dt< 0

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Monthly mean surface energy balance during stable conditions

MonthNblocks

10 minutes

H(Wm-2)

LE(Wm-2)

-G0

(Wm-2)LWnet

(Wm-2)Res

(Wm-2)

Jan 797 -4.9 -0.7 12.0 52.2 34.6

Feb 770 -7.7 0.0 13.0 55.6 34.9

Mar 1240 -5.9 0.8 12.7 52.2 34.4

Apr 1393 -6.1 1.6 14.1 49.8 31.2

May 1150 -6.5 0.4 14.5 48.5 27.9

Jun 1154 -8.4 1.8 15.9 48.3 25.9

Jul 996 -11.0 0.9 14.3 46.6 22.2

Aug 1297 -7.8 1.3 12.5 47.0 28.1

Sep 1755 -7.7 -0.4 14.8 47.7 24.7

Oct 1047 -8.2 -0.5 11.0 48.3 28.5

Nov 945 -4.7 -2.6 12.5 49.9 30.1

Dec 1222 -4.7 -1.2 13.4 52.5 33.3

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Monthly mean surface energy balance during stable conditions

MonthNblocks

10 minutes

H(Wm-2)

LE(Wm-2)

-G0

(Wm-2)LWnet

(Wm-2)Res

(Wm-2)

Jan 797 -4.9 -0.7 12.0 52.2 34.6

Feb 770 -7.7 0.0 13.0 55.6 34.9

Mar 1240 -5.9 0.8 12.7 52.2 34.4

Apr 1393 -6.1 1.6 14.1 49.8 31.2

May 1150 -6.5 0.4 14.5 48.5 27.9

Jun 1154 -8.4 1.8 15.9 48.3 25.9

Jul 996 -11.0 0.9 14.3 46.6 22.2

Aug 1297 -7.8 1.3 12.5 47.0 28.1

Sep 1755 -7.7 -0.4 14.8 47.7 24.7

Oct 1047 -8.2 -0.5 11.0 48.3 28.5

Nov 945 -4.7 -2.6 12.5 49.9 30.1

Dec 1222 -4.7 -1.2 13.4 52.5 33.3

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Dew formation downward vertical humidity transport

Problems

- eddy correlation humidity flux at 5 m is negligibly small

- large residual in surface energy balance

Relevance

- Testing schemes (TKE, EDMF, etc) against observations

- Site used for GABLS3 case

- Humidity important for fog formation

Question

- Are the measured latent heat fluxes in accord with observed humidity tendencies from

Cabauw tower?

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Example: humidity tendencies from Cabauw tower

qsat,sfc

2m

10m

80 m

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Mean humidity tendencies (all selected SBLs)

Significant mean tendencies near the surface

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Mean humidity tendencies at 2m as a function of wind direction

Negative humidity tendency for any prevailing mean wind direction

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Tendencies of the mean humidity at 2m and the surface saturation specific humidity

Surface cooling causes downgradient humidity flux

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Mean humidity tendencies as a function of the bulk Richardson number

Tendencies even for very stable conditions

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Ditches are another local source of moisture

Courtesy Kees FloorCourtesy Adriaan Schuitmaker

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Dispersion of a passive scalar in a stable boundary layer at Cabauw

Field experiment (measuring vertical velocities with laser technique) by Petra Kroon, Harm Jonker, Adriaan Schuitmaker and others (TU Delft)

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Sources dew formation

1. Vertical turbulent transport from atmospheric column

2. Condensation of moisture evaporated from ditches

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Dew research in Wageningen (Jacobs et al.)

Wageningen dew fall corresponds to a mean latent heat flux of about 10 Wm-2

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Conclusions

1. Surface energy imbalance partly due to "missing" latent heat flux

- instrument wetting

- measurement height 5 m

- small turbulent fluctuations

2. Dew fall from

- atmospheric column

- evaporated moisture from numerous ditches

3. We expect similar dew fall as in Wageningen (about 50 km from

Cabauw)

- latent heat flux LE≈-10Wm-2 (Jacobs et al. 2006)

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Monthly mean humidity tendencies (g/kg/hr)

Month sfc 2m 10m 20m 40m 80m 140m 200m LE(Wm-

2)

Jan -0.23 -0.19 -0.07 -0.03 -0.02 -0.00 -0.01 0.00 -2.6

Feb -0.23 -0.15 -0.05 -0.04 -0.03 -0.03 -0.02 -0.04 -5.3

Mar -0.28 -0.18 -0.06 -0.04 -0.02 -0.02 -0.02 -0.02 -4.3

Apr -0.48 -0.20 -0.05 -0.02 -0.01 -0.01 -0.02 -0.02 -3.9

May -0.68 -0.22 -0.04 0.00 0.01 0.01 0.00 -0.04 -1.9

Jun -0.69 -0.17 -0.01 0.02 0.04 0.03 0.01 -0.02 1.2

Jul -0.85 -0.25 -0.08 -0.04 -0.01 0.02 -0.01 -0.06 -4.0

Aug -0.76 -0.31 -0.12 -0.09 -0.04 0.00 -0.05 -0.06 -8.3

Sep -0.71 -0.33 -0.09 -0.06 -0.03 -0.04 -0.06 -0.05 -9.4

Oct -0.64 -0.36 -0.15 -0.11 -0.08 -0.07 -0.06 -0.05 -12.5

Nov -0.49 -0.33 -0.13 -0.08 -0.05 -0.05 -0.06 -0.06 -10.5

Dec -0.27 -0.25 -0.09 -0.04 -0.03 -0.02 -0.03 -0.01 -5.4

correspondingflux