Jieying Ding, Ujjwal Kumar, Henk Eskes , Henk Klein- Baltink

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A comparison of air quality simulated by LOTO-EUROS driven by Harmonie and ECMWF using observations from Cabauw Jieying Ding, Ujjwal Kumar, Henk Eskes, Henk Klein-Baltink

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A comparison of air quality simulated by LOTO-EUROS driven by Harmonie and ECMWF using observations from Cabauw. Jieying Ding, Ujjwal Kumar, Henk Eskes , Henk Klein- Baltink. Outline of our talk. The motivation and background The model set up Comparison : - PowerPoint PPT Presentation

Transcript of Jieying Ding, Ujjwal Kumar, Henk Eskes , Henk Klein- Baltink

Page 1: Jieying  Ding,  Ujjwal  Kumar,  Henk Eskes ,  Henk  Klein- Baltink

A comparison of air quality simulated by LOTO-EUROS driven by Harmonie and

ECMWF using observations from Cabauw

Jieying Ding, Ujjwal Kumar, Henk Eskes, Henk Klein-Baltink

Page 2: Jieying  Ding,  Ujjwal  Kumar,  Henk Eskes ,  Henk  Klein- Baltink

The motivation and background

The model set up Comparison :

Meteorological variables Air quality variables

Conclusions

Outline of our talk

Page 3: Jieying  Ding,  Ujjwal  Kumar,  Henk Eskes ,  Henk  Klein- Baltink

Current air quality forecasts by LOTOS-EUROS is driven by ECMWF meteorology which is available at coarse resolution (~15 km)

HARMONIE meteorology is available at a very high resolution at ~2.5 km. HARMONIE is the new high resolution numerical weather model operational at KNMI since 7 Dec 2011.

The purpose of this study is to evaluate LOTOS-EUROS driven by HARMONIE and ECMWF meteorology using (Cabauw) observations

Motivation and Background

Page 4: Jieying  Ding,  Ujjwal  Kumar,  Henk Eskes ,  Henk  Klein- Baltink

What are the differences of meteorological variables between ECMWF and Harmonie?

What are the differences of air quality simulations using two meteorological drivers?

How do the differences of meteorological conditions affect the air quality in LOTOS-EUROS?

Research questions

Page 5: Jieying  Ding,  Ujjwal  Kumar,  Henk Eskes ,  Henk  Klein- Baltink

The main meteorological variables affect air quality processes in LOTOS-EUROS

Page 6: Jieying  Ding,  Ujjwal  Kumar,  Henk Eskes ,  Henk  Klein- Baltink

Time : June to August , 2012 LOTOS-EUROS was run for the target domain

(00E- 110E, 490N- 550N) at the high resolution (~3.5 km) using HARMONIE meteorology (available at 2.5 km resolution)

LOTOS-EUROS was also run for the target domain at ~3.5 km resolution using ECMWF meteorology (available at ~15 km resolution).

Chemical boundary conditions are from MACC:

Model set up

Page 7: Jieying  Ding,  Ujjwal  Kumar,  Henk Eskes ,  Henk  Klein- Baltink

Meteo ( KNMI ) : 10 stations Air quality ( LML of RIVM ) : 8 regional background

stations

Observation data

Page 8: Jieying  Ding,  Ujjwal  Kumar,  Henk Eskes ,  Henk  Klein- Baltink

Surface temperature

Comparison: Meteorological variables

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Relative humidity

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Wind speed

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Boundary layer height

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O3

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The surface temperature difference between two meteorological models is around 1.5 to 2 K.

The differences of surface relative humidity, wind speed between two models are large, at least above 10%.

The boundary layer height simulated by Harmonie is low compared to observations.

Apart from the boundary layer height, it is hard to show which meteo model is better.

The difference in air quality results between the two simulations is large. The RMS difference for ozone is 20ug/m3.

Conclusions

Page 14: Jieying  Ding,  Ujjwal  Kumar,  Henk Eskes ,  Henk  Klein- Baltink

Any questions?