@article{
 title = {Alkyl nitrate and selected halocarbon measurements at Mauna Loa Observatory, Hawaii},
 type = {article},
 year = {1992},
 keywords = {Air,Air mass source,Alkyl nitrate,Atmosphere,Atmospheric composition,Boundary layer,Bromoform,Chemical composition,Concentration,Diurnal variation,Halocarbon,Hawaii,Mauna Loa Observatory,North Pacific,Organic compounds,Perchlorethylene,Slope circulation,Synoptic-scale circulation,Troposphere,ad 1988 05,ad 1988 06,mlopex},
 pages = {10331-10348},
 volume = {97},
 id = {7eda4a91-6cd8-3a24-9045-05cd84b80459},
 created = {2015-02-12T00:34:11.000Z},
 file_attached = {false},
 profile_id = {81af7548-db00-3f00-bfa0-1774347c59e1},
 group_id = {63e349d6-2c70-3938-9e67-2f6483f6cbab},
 last_modified = {2015-02-12T20:19:21.000Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 source_type = {Journal Article},
 notes = {<m:note>Article</m:note>},
 abstract = {Measurements of >or=C/sub 3/ alkyl nitrates, perchlorethylene, and bromoform were made during the Mauna Loa Observatory Photochemistry Experiment (MLOPEX). The median mixing ratios of these compounds in free tropospheric air (3.4 km) were 2.3, 3.2, and 0.20 pptv, respectively. A diurnal variation in the concentration of these compound at Mauna Loa was driven by the local upslope/downslope circulation and by differences in the concentration of these species between the boundary layer and the free troposphere. Longer term variation was closely related to synoptic-scale circulation of the North Pacific and to differences in the sources of air masses reaching Hawaii.},
 bibtype = {article},
 author = {Atlas, E and Schauffler, S M and Merrill, J T and Hahn, C J and Ridley, B and Walega, J and Greenberg, J and Heidt, L and Zimmerman, P},
 journal = {Journal of Geophysical Research},
 number = {D10}
}

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