@article{
 title = {HOx concentrations and OH reactivity observations in New York City during PMTACS-NY2001},
 type = {article},
 year = {2003},
 identifiers = {[object Object]},
 keywords = {deciduous forest,field campaign,hydroperoxy radical,hydroxyl radical,hydroxyl radicals,laser-induced fluorescence,measurement,mechanism,nighttime hydroxyl,north-western greece/,ozone,pem-tropics,photochemistry experiment,tropospheric oh,urban environment},
 pages = {3627-3637},
 volume = {37},
 websites = {<Go to ISI>://000184353300002},
 id = {0910ee90-49bd-346b-a6c2-d035822ae286},
 created = {2015-02-12T14:34:45.000Z},
 file_attached = {false},
 profile_id = {81af7548-db00-3f00-bfa0-1774347c59e1},
 group_id = {63e349d6-2c70-3938-9e67-2f6483f6cbab},
 last_modified = {2015-02-12T20:19:47.000Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 source_type = {Journal Article},
 language = {English},
 notes = {<m:note>704RH<m:linebreak/>Times Cited:56<m:linebreak/>Cited References Count:43</m:note>},
 abstract = {Hydroxyl (OH) and hydroperoxy (HO2) radicals (collectively called HOx) were measured by a laser-induced fluorescence instrument during the PMTACS-NY (PM2.5 Technology Assessment and Characterization Study-New York) intensive campaign in New York City in summer 2001. Measurement results for OH and HO2 are presented for the month-long study. The detection limits were about 3.0 x 10(5) cm(-3) for OH and 2.5 x 10(6) cm(-3) (similar to0.1 ppt) for HO2 with a 1-min integration time and a 2sigma confidence level. The daytime maximum concentrations were 5-20 x 10(6) cm(-3) for OH and 0.4-6 x 10(8) cm(-3) (2-24 pptv) for HO2, usually appearing later than the peak of ozone photolysis frequency, J((OD)-D-1). Relative high OH and HO2 persisted into early evening and were frequently observed during nighttime. The ratios of HO2 to OH were typically between 5 and 40, which are smaller than those obtained in relatively clean environments. The OH reactivity, measured by an instrument named total OH loss rate measurement was on average 19+/-3 s(-1) in this urban environment. It was the highest in the morning and the lowest in the afternoon. The comparison of measured OH and HO2 with model calculations is given in a companion paper (OH and HO2 chemistry in the urban atmosphere of New York City, Atmospheric Environment (2003a) this issue). (C) 2003 Elsevier Ltd. All rights reserved.},
 bibtype = {article},
 author = {Ren, X R and Harder, H and Martinez, M and Lesher, R L and Oliger, A and Shirley, T and Adams, J and Simpas, J B and Brune, W H},
 journal = {Atmospheric Environment},
 number = {26}
}

{"_id":"XYg5uQLAsiPTtJzdn","bibbaseid":"ren-harder-martinez-lesher-oliger-shirley-adams-simpas-etal-hoxconcentrationsandohreactivityobservationsinnewyorkcityduringpmtacsny2001-2003","downloads":0,"creationDate":"2017-01-12T21:32:07.668Z","title":"HOx concentrations and OH reactivity observations in New York City during PMTACS-NY2001","author_short":["Ren, X., R.","Harder, H.","Martinez, M.","Lesher, R., L.","Oliger, A.","Shirley, T.","Adams, J.","Simpas, J., B.","Brune, W., H."],"year":2003,"bibtype":"article","biburl":null,"bibdata":{"title":"HOx concentrations and OH reactivity observations in New York City during PMTACS-NY2001","type":"article","year":"2003","identifiers":"[object Object]","keywords":"deciduous forest,field campaign,hydroperoxy radical,hydroxyl radical,hydroxyl radicals,laser-induced fluorescence,measurement,mechanism,nighttime hydroxyl,north-western greece/,ozone,pem-tropics,photochemistry experiment,tropospheric oh,urban environment","pages":"3627-3637","volume":"37","websites":"<Go to ISI>://000184353300002","id":"0910ee90-49bd-346b-a6c2-d035822ae286","created":"2015-02-12T14:34:45.000Z","file_attached":false,"profile_id":"81af7548-db00-3f00-bfa0-1774347c59e1","group_id":"63e349d6-2c70-3938-9e67-2f6483f6cbab","last_modified":"2015-02-12T20:19:47.000Z","read":false,"starred":false,"authored":false,"confirmed":"true","hidden":false,"source_type":"Journal Article","language":"English","notes":"<m:note>704RH<m:linebreak/>Times Cited:56<m:linebreak/>Cited References Count:43</m:note>","abstract":"Hydroxyl (OH) and hydroperoxy (HO2) radicals (collectively called HOx) were measured by a laser-induced fluorescence instrument during the PMTACS-NY (PM2.5 Technology Assessment and Characterization Study-New York) intensive campaign in New York City in summer 2001. Measurement results for OH and HO2 are presented for the month-long study. The detection limits were about 3.0 x 10(5) cm(-3) for OH and 2.5 x 10(6) cm(-3) (similar to0.1 ppt) for HO2 with a 1-min integration time and a 2sigma confidence level. The daytime maximum concentrations were 5-20 x 10(6) cm(-3) for OH and 0.4-6 x 10(8) cm(-3) (2-24 pptv) for HO2, usually appearing later than the peak of ozone photolysis frequency, J((OD)-D-1). Relative high OH and HO2 persisted into early evening and were frequently observed during nighttime. The ratios of HO2 to OH were typically between 5 and 40, which are smaller than those obtained in relatively clean environments. The OH reactivity, measured by an instrument named total OH loss rate measurement was on average 19+/-3 s(-1) in this urban environment. It was the highest in the morning and the lowest in the afternoon. The comparison of measured OH and HO2 with model calculations is given in a companion paper (OH and HO2 chemistry in the urban atmosphere of New York City, Atmospheric Environment (2003a) this issue). (C) 2003 Elsevier Ltd. All rights reserved.","bibtype":"article","author":"Ren, X R and Harder, H and Martinez, M and Lesher, R L and Oliger, A and Shirley, T and Adams, J and Simpas, J B and Brune, W H","journal":"Atmospheric Environment","number":"26","bibtex":"@article{\n title = {HOx concentrations and OH reactivity observations in New York City during PMTACS-NY2001},\n type = {article},\n year = {2003},\n identifiers = {[object Object]},\n keywords = {deciduous forest,field campaign,hydroperoxy radical,hydroxyl radical,hydroxyl radicals,laser-induced fluorescence,measurement,mechanism,nighttime hydroxyl,north-western greece/,ozone,pem-tropics,photochemistry experiment,tropospheric oh,urban environment},\n pages = {3627-3637},\n volume = {37},\n websites = {<Go to ISI>://000184353300002},\n id = {0910ee90-49bd-346b-a6c2-d035822ae286},\n created = {2015-02-12T14:34:45.000Z},\n file_attached = {false},\n profile_id = {81af7548-db00-3f00-bfa0-1774347c59e1},\n group_id = {63e349d6-2c70-3938-9e67-2f6483f6cbab},\n last_modified = {2015-02-12T20:19:47.000Z},\n read = {false},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n source_type = {Journal Article},\n language = {English},\n notes = {<m:note>704RH<m:linebreak/>Times Cited:56<m:linebreak/>Cited References Count:43</m:note>},\n abstract = {Hydroxyl (OH) and hydroperoxy (HO2) radicals (collectively called HOx) were measured by a laser-induced fluorescence instrument during the PMTACS-NY (PM2.5 Technology Assessment and Characterization Study-New York) intensive campaign in New York City in summer 2001. Measurement results for OH and HO2 are presented for the month-long study. The detection limits were about 3.0 x 10(5) cm(-3) for OH and 2.5 x 10(6) cm(-3) (similar to0.1 ppt) for HO2 with a 1-min integration time and a 2sigma confidence level. The daytime maximum concentrations were 5-20 x 10(6) cm(-3) for OH and 0.4-6 x 10(8) cm(-3) (2-24 pptv) for HO2, usually appearing later than the peak of ozone photolysis frequency, J((OD)-D-1). Relative high OH and HO2 persisted into early evening and were frequently observed during nighttime. The ratios of HO2 to OH were typically between 5 and 40, which are smaller than those obtained in relatively clean environments. The OH reactivity, measured by an instrument named total OH loss rate measurement was on average 19+/-3 s(-1) in this urban environment. It was the highest in the morning and the lowest in the afternoon. The comparison of measured OH and HO2 with model calculations is given in a companion paper (OH and HO2 chemistry in the urban atmosphere of New York City, Atmospheric Environment (2003a) this issue). (C) 2003 Elsevier Ltd. All rights reserved.},\n bibtype = {article},\n author = {Ren, X R and Harder, H and Martinez, M and Lesher, R L and Oliger, A and Shirley, T and Adams, J and Simpas, J B and Brune, W H},\n journal = {Atmospheric Environment},\n number = {26}\n}","author_short":["Ren, X., R.","Harder, H.","Martinez, M.","Lesher, R., L.","Oliger, A.","Shirley, T.","Adams, J.","Simpas, J., B.","Brune, W., H."],"urls":{"Website":"<Go to ISI>://000184353300002"},"bibbaseid":"ren-harder-martinez-lesher-oliger-shirley-adams-simpas-etal-hoxconcentrationsandohreactivityobservationsinnewyorkcityduringpmtacsny2001-2003","role":"author","keyword":["deciduous forest","field campaign","hydroperoxy radical","hydroxyl radical","hydroxyl radicals","laser-induced fluorescence","measurement","mechanism","nighttime hydroxyl","north-western greece/","ozone","pem-tropics","photochemistry experiment","tropospheric oh","urban environment"],"downloads":0},"search_terms":["hox","concentrations","reactivity","observations","new","york","city","during","pmtacs","ny2001","ren","harder","martinez","lesher","oliger","shirley","adams","simpas","brune"],"keywords":["deciduous forest","field campaign","hydroperoxy radical","hydroxyl radical","hydroxyl radicals","laser-induced fluorescence","measurement","mechanism","nighttime hydroxyl","north-western greece/","ozone","pem-tropics","photochemistry experiment","tropospheric oh","urban environment"],"authorIDs":[]}