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Scientific Theme: Advanced Modeling and Observing Systems

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<strong>Scientific</strong> <strong>Theme</strong>: Planetary Metabolism<br />

<strong>Scientific</strong> <strong>Theme</strong>: PLANETARY METABOLISM<br />

PM-01: Biosphere-Atmosphere Interactions<br />

CSD07: Biosphere-Atmosphere Exchange<br />

PM-02: Response of Natural <strong>Systems</strong> to Perturbations<br />

NGDC07: Anthropogenic Remote Sensing<br />

CSD07: Biosphere-Atmosphere Exchange<br />

PM-01: Biosphere-Atmosphere Interactions<br />

GOAL:<br />

Gain an improved underst<strong>and</strong>ing of the role that the exchange of gases between the surface <strong>and</strong> the atmosphere<br />

plays in shaping regional climate <strong>and</strong> air quality.<br />

MILESTONE CSD07.1:<br />

Determine the impact of the 2004 forest fires in Alaska <strong>and</strong> western Canada on the atmosphere<br />

over North America.<br />

ACCOMPLISHMENTS FOR CSD07.1:<br />

During aircraft measurements in 2004 over the northeastern United States, large forest fires were burning in Alaska<br />

<strong>and</strong> western Canada, <strong>and</strong> the emissions were regularly observed over eastern Canada <strong>and</strong> the northeastern U.S.<br />

Using measurements of acetonitrile (CH3CN), a unique tracer for forest-fire emissions, CIRES scientists were able<br />

to detect the emissions <strong>and</strong> compare the observations to the output from the Lagrangian transport model Flexpart. In<br />

general, Flexpart reproduced the observations very well, in particular when the emissions were released in the model<br />

not at the surface but at an altitude of several kilometers, indicating the importance of pyro-convection.<br />

The measurement results were used to estimate the contribution of forest-fire emissions to the carbon monoxide<br />

(CO) observed over the northeastern U.S. Using acetonitrile as a tracer for forest-fire emissions <strong>and</strong> chloroform as a<br />

tracer for urban emissions, scientists were able to separate the contribution of these sources to CO. Averaged over<br />

the study period, forest-fire CO contributed 30% <strong>and</strong> urban CO 70% of the enhancements over the continental CO<br />

background: Urban CO dominated in the boundary layer, whereas in the free troposphere the contributions from<br />

urban <strong>and</strong> forest fire CO were about equal. The observations in the boundary layer were consistent with those made<br />

from the R/V Ronald H. Brown in the Gulf of Maine. The source attribution was compared with the output from the<br />

Flexpart model. In general, there was a good qualitative agreement between urban CO in the measurements <strong>and</strong> the<br />

model. However, the model over-predicted the observed urban CO, indicating that emissions inventories for this<br />

trace gas may be too high as observed by others. The agreement between measured <strong>and</strong> modeled forest-fire CO was<br />

also quite good; in this case, the model reproduced the measurements quantitatively, indicating that emissions from<br />

forest fires are accurately represented in the inventories. This study allows us to estimate the total emissions of CO<br />

due to forest fires in Alaska <strong>and</strong> western Canada as 22 Tg during the measurement period in 2004, in quite good<br />

agreement with a previous study that used satellite data for CO <strong>and</strong> an inverse-model estimate of the emission<br />

sources.<br />

PM-02: Response of Natural <strong>Systems</strong> to Perturbations<br />

NGDC07: Anthropogenic Remote Sensing<br />

GOAL:<br />

Provide spatial <strong>and</strong> temporal depictions of human activities based on satellite detection <strong>and</strong> mapping of population<br />

centers, fires, gas flares, <strong>and</strong> heavily lit fishing boats.<br />

MILESTONE NGDC07.1:<br />

Produce the first global ~1 kilometer map of the density of constructed impervious surface areas.<br />

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