Biogenic Emissions in Southeast Texas

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Presentation transcript:

Biogenic Emissions in Southeast Texas Ji Hee Song Environmental and Water Resources Engineering University of Texas at Austin

Outline Characteristics of Isoprene Meteorological data from the TexAQS 2000 episode Biogenic emission model Time varying distribution of Isoprene emissions Comparison of emission by different model version My first task was to see the performance of CAMx model, comparing with observed data from NOAA aircraft. The time period of my interest was from August 25 to September 1 in 2000.

Isoprene Highly reactive hydrocarbon Mostly emitted by trees and plants ; oaks, popular, etc. Isoprene + NOx  Ozone formation

GloBEIS 3.0 (Global Biosphere Emissions and Interactions System version 3.0)

Inputs to GloBEIS 3.0 Meteorology based on MM5 outputs Satellited based cloud cover data Texas specific landcover data

Hourly Biogenic Emissions in tons Strongly related to sunlight year day hour Isoprene TMT OVC NOx 2000 238 31 22 2.5 1 30 2 29 21 2.4 3 20 4 28 5 27 19 2.3 6 26 7 73 8 147 39 2.6 9 206 44 2.8 10 253 48 34 2.9 11 292 52 37 3.1 12 319 55 3.3 13 328 57 40 3.4 14 316 41 3.5 15 290 58 3.6 16 234 17 146 18 53 47 33 42 38 35 25 2.7 23 24 Daily Totals 2603 999 713 68.6 Hourly Biogenic Emissions in tons Strongly related to sunlight For the temperature and cloud cover sensitivity, modified GloBEIS 2 was used. First the temperature,

Distribution on the ArcMap Isoprene emissions w/ Graduated colors Units : g/each cell

Hourly Based Isoprene Distribution 7:00 am 12:00 pm However, these four graphs show that varied temperature and cloud cover input data don’t shift the result much. Which indicates that the isoprene concentration is not very sensitive to temperature and cloud cover. 3:00 pm 5:00 pm

Comparison of model results (GloBEIS 3.0 vs. Modified GloBEIS 2.0) Older version of GloBEIS underpredicted the isoprene emissions The conclusion. Model is well predicted the isoprene concentration, however, the discrepancy is due to the meteorological data such as rapid changing wind direction. And anthropogenic sources, which can not be predicted by the model. And certain types of landcover data.

Special Thanks to.. Dr. David Maidment from University of Texas, Austin Dr. David T. Allen from University of Texas, Austin Alex Guenther from NCAR Christine Wiedinmyer from NCAR Mark Estes from ENVIRON Yosuke Kimura from University of Texas, Austin Matt Russell from University of Texas, Austin Gary McGaughey from University of Texas, Austin Special thanks to …

Questions?