Development, evaluation, and application of GEOS-Chem driven by CCSM3 meteorological fields Presenter: Daeok (Daniel) Youn Atmospheric Chemistry Modeling.

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Presentation transcript:

Development, evaluation, and application of GEOS-Chem driven by CCSM3 meteorological fields Presenter: Daeok (Daniel) Youn Atmospheric Chemistry Modeling Group School of Earth and Environmental Sciences, Seoul National University, Seoul, , Korea, Republic of 4 th GEOS-Chem USERS’ MEETING Maxwell-Dworkin building, room G115 Harvard University, Cambridge, MA, April 7, 2009

Global CO B40 December CO emissions inventory over Globe and Asia Recent changes in Emissions by sector SO2 vs. CO Objective and Background

Simulated seasonal surface O 3 for 2001: GEOS-Chem/CCSM3 vs. GEOS-Chem/GEOS-4 GEOS-Chem/CCSM-3 GEOS-Chem/GEOS-4 Both simulations produced consistent seasonal and spatial patterns of ozone concentrations in surface air.

Comparison between Simulated and Sonde O 3 at 800 hPa CCSM-3 GEOS-4 Both simulations reproduced ozone sonde observation relatively well.

Comparison between Simulated and Sonde O 3 at 500 hPa CCSM-3 GEOS-4

Comparison between Simulated and Sonde O 3 at 300 hPa CCSM-3 GEOS-4

GEOS-Chem driven by CCSM3(CAM3-CLM3)+DGVM An application of off-line coupling between GEOS- Chem and CCSM3 for to look at the impact of BVOC emissions on air quality in East Asia

Simulated Surface Variable in 2000 and 2006 LAI in East Asia PAR in East Asia 2-m air Temperature Decreases in LAI in northeast China correspond to the increases in surface air temperature in the same region.

MODIS LAI & NCEP-R2 T 2m air (Observation) 2m air Temp. NCEP-R2 LAI in East Asia MODIS-BU Observations show opposite results from the model in LAI and air temp. the negative correlation between changes in LAI and surface holds both for obs. And model

Simulated Surface Isoprene and resulting Ozone Change Ozone change is likely related to the distribution of isoprene at the near surface over East Asia, esp. east China, for the two different years. GEOS-Chem/CCSM3+DGVM GEOS-Chem/GEOS-4

Additional slides

Change in Surface Variables: GEOS-4 PAR in East Asia 2-m air Temperature LAI in East Asia

BVOC emissions by CCSM3-DGVM and GEOS-Chem/CCSM3-DGVM Isoprene emissions from CCSM3-DGVM and GEOS-Chem are in general agreement in that lower isoprene emissions in mid- to high- latitudes over most of Northeast Asia for 2005 and higher emissions in tropics over Southeast Asia are shown. Vegetation maps are different! GEOS-Chem/ CCSM3-DGVM CCSM3-CLM3

Bonan et al. (2003) CAM3-CLM3 with DGVM Interactive Vegetation Observed SST for Sitch et al. (2003) Meteorological Fields, Land Surface Variables, Tsfc, LAI, and PAR

Observation Default CCSM3CCSM3+DGVM Comparison between Observed vs. Simulated Plant Type Functions (PFT)

CAM3-CLM3: 1) with prescribed vegetation and 2) interactive vegetation (DGVM) GEOS-Chem driven by the CAM3-CLM3 MODELS CAM3-CLM3 with DGVM 500 year control SST Climatology CAM3-CLM3 Prescribed Vegetation CAM3-CLM3 with DGVM Interactive Vegetation Output: surface component (PFT, LAI, SAI, Height) Initial condition Surface data set 10 PFT and 1 LAI in a grid 14 PFT and 10 LAI in a grid Observed SST for GEOS-Chem/CCSM3 Observed SST for Air Quality (O3 and Aerosol)