Development of Alternative Methods For Estimating Dry Deposition Velocity In CMAQ

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Development of Alternative Methods For Estimating Dry Deposition Velocity In CMAQ

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UNC-CH. Development of Alternative Methods For Estimating Dry Deposition Velocity In CMAQ. UNC-CH. Kiran Alapaty University of North Carolina at Chapel Hill. Dev Niyogi North Carolina State University. Sarav Arunachalam Andrew Holland Kimberly Hanisak - PowerPoint PPT Presentation

Transcript of Development of Alternative Methods For Estimating Dry Deposition Velocity In CMAQ

Page 1: Development of  Alternative Methods  For Estimating Dry Deposition Velocity  In CMAQ

Development of Alternative Methods

For EstimatingDry Deposition Velocity

In CMAQ

Page 2: Development of  Alternative Methods  For Estimating Dry Deposition Velocity  In CMAQ

Kiran AlapatyUniversity of North Carolina at Chapel Hill

Dev NiyogiNorth Carolina State University

Sarav ArunachalamAndrew HollandKimberly HanisakUniversity of North Carolina at Chapel Hill

Marvin Wesely (Posthumous)Argonne National Laboratory

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Dry Deposition Velocity estimation

INTRODUCTION

1 cbad RRRV

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Time Series of Dom Avg ResistancesL

og

Sca

le

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• Rc sum of several resistance for theSoil-vegetation Continuum.

• One of them is the Stomatal

Resistancefor a gas (Rsg)

• Rsg is proportional to Rsw

• Rsw Plays an important role in Land

surface Modeling.

Relation of Rc to Stomatal Resistance

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• Stomatal Resistance:

A key Parameter in Land surface Modeling

• Why ? Stomata Controls Water Vapor Exchange

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Stoma (pore) through which CO2 enters for use in Photosynthesis; releases O2 & H2O Depending on the

applications, Rs is modeled using a variety of forcings.

For environmental Applications:

- Wesely scheme

- Jarvis scheme

- Ball–Berry scheme

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• JARVIS method is used in many LSMs(traditional in Met Models)

• WESELY method is used many AQMs

• Micro-Met and GCMs use Photosynthesis/CO2 assimilation

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Stomatal Resistance Formulations

WESELY

JARVIS

Ball-Berry (GEM)

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• JARVIS & WESELY methods Based on Minimum Stom. Resist.

• Ball – Berry method Based on Photosynthesis approach

(e.g., Farquhar, Collatz, Niyogi et al. ,

Wu et al.)

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WESELY

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JARVIS

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GEM

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OBJECTIVES

Introduce and evaluate a Photosynthesis-based Vegetation Model for estimating stomatal resistance in MM5 and deposition velocity in CMAQ

Intercompare results from Jarvis-, Wesely-, GEM (photosynthesis) – type methods

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Methodology

Photosynthesis Model Development:• Testing in 1D mode• Integrate GEM, Wesely, and Jarvis within a LSM• Couple Unified LSM (with three schemes) to MM5• Develop 3D model simulations using MM5 • Use Vd estimates from the three schemes in CMAQ

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GEM development results1-D Model Results

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MM5 Simulation Details

Simulation Domain – 36 km grids for TexasAir Quality Study

• 28 Layers• MRF ABL• Noah LSM• Grell • RRTM • FDDA• 5.5 days• 23 Aug 2000 • TDL hourly Data

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• Discussion of MM5 / Unified Noah

(with three Rs schemes) model Results

– Model performance statistics with surface observations

– Model diagnostics for the 3 schemes (surface parameters – energy fluxes, temperature, and estimated Rs values,….)

Will Present:

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Nu

mb

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Surface Observations used in STATS

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OBS WES JAR GEM

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K)

Simulation Time (h)

Time Series for Temp1.5

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Temperature Bias (Model – Obs)

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Simulation Time (h)

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Mix

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g k

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Simulation Time (h)

Mod. Lowest Vs Obs. Surface Level Qv

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Simulation Time (h)

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Diagnostic & Other Parameters

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Land Domain Avg. ABL Depths (m)

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recip

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Land Domain Avg. TRF (cm/h)

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Hea

t F

lux (

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Simulation Time (h)

Canopy Conductance

Sfc. Latent Heat Flux

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Sfc. Sensible Heat Flux

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Agriculture Land (26%)

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tan

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Simulation Time (h)

(LU=3)

RANGE Land (34%)

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Land Use Patterns

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ABL Depths at 20 UTC

WES JAR GEM

(Acquire Lidar & other ABL obs)

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TRF per hour

WES JAR GEM

(Acquire Stage IV Radar)

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Cloud Fraction

WES JAR GEM

(Acquire GOES)

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MCIP was modified to generate Dep Vel fieldsusing M3-DryDepfor CMAQ

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WES JAR GEM

Dep. Vel. for Ozone at 22 UTC

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WES JAR GEM

Dep. Vel. for NO2 at 22 UTC

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Domain Averaged Vd for O3

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We are still doing analysis of MET fields

Once completed, we willperform CMAQ simulationsby keeping all MET fields identical except Dep Vel

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• These Schemes are also being tested in WRF model

• WRF-CMAQ driver is alsoUnder construction