@article{
 title = {Trajectory analysis of source regions influencing the south greenland ice-sheet during the dye-3 gas and aerosol sampling program},
 type = {article},
 year = {1993},
 pages = {2739-2749},
 volume = {27},
 id = {a3cd914d-57b0-3597-a238-a82659b3bbfb},
 created = {2014-10-08T16:28:18.000Z},
 file_attached = {false},
 profile_id = {363623ef-1990-38f1-b354-f5cdaa6548b2},
 group_id = {02267cec-5558-3876-9cfc-78d056bad5b9},
 last_modified = {2017-03-14T17:32:24.802Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Davidson:AEPAGT:1993d},
 source_type = {article},
 private_publication = {false},
 abstract = {Backward air mass trajectories for Dye 3, Greenland
(elevation 2.5 km) show source regions that vary with season: the
direction of greatest transport distance is from the southwest in
fall, west in winter, and northwest in spring; the trajectories in
summer do not show a strong preferred direction. Based on 5 d
transit times, the trajectories in fall suggest the importance of
North America as a potential source region, with occasional
trajectories from western Europe, The trajectories in spring,
especially in April, suggest Eurasia (transport over the Pole),
eastern North America, and western Europe as potential source
regions. Less transport of chemical constituents to Dye 3 is
expected in summer when transport distances are shorter. Although
some long-range transport to Greenland occurs in winter, the
stability of the atmosphere over the ice sheet at this time of year
is likely to limit the delivery of chemical constituents to the
surface. Sources outside of these regions can also influence Dye 3
if transit times longer than 5 d are considered. These results are
in contrast to trajectories reported by others for sea-level arctic
locations such as Barrow, Alaska and Mould Bay, Canada, where
transport over the Pole from Eurasia is responsible for high
chemical species concentrations over much of the winter and early
spring. Overall, the trajectories are consistent with aerosol
chemical data for this time period at Dye 3 reported by several
investigators, showing peak concentrations in spring and fall.
C1 CNRS,GLACIOL & GEOPHYS ENVIRONNEMENT LAB,F-38402 ST MARTIN
DHERES,FRANCE. ATMOSPHER ENVIRONM SERV,DOWNSVIEW M3H 5T4,ON,CANADA.
UNIV NEVADA,DESERT RES INST,CTR ATMOSPHER SCI,RENO,NV 89506.},
 bibtype = {article},
 author = {Davidson, C I and Jaffrezo, J L and Small, M J and Summers, P W and Olson, M P and Borys, R D},
 journal = {Atmos Environ Pt A-Gen Top}
}

{"_id":{"_str":"5411bfbb480d3bb058002add"},"__v":0,"authorIDs":[],"author_short":["Davidson, C., I.","Jaffrezo, J., L.","Small, M., J.","Summers, P., W.","Olson, M., P.","Borys, R., D."],"bibbaseid":"davidson-jaffrezo-small-summers-olson-borys-trajectoryanalysisofsourceregionsinfluencingthesouthgreenlandicesheetduringthedye3gasandaerosolsamplingprogram-1993","bibdata":{"title":"Trajectory analysis of source regions influencing the south greenland ice-sheet during the dye-3 gas and aerosol sampling program","type":"article","year":"1993","pages":"2739-2749","volume":"27","id":"a3cd914d-57b0-3597-a238-a82659b3bbfb","created":"2014-10-08T16:28:18.000Z","file_attached":false,"profile_id":"363623ef-1990-38f1-b354-f5cdaa6548b2","group_id":"02267cec-5558-3876-9cfc-78d056bad5b9","last_modified":"2017-03-14T17:32:24.802Z","read":false,"starred":false,"authored":false,"confirmed":"true","hidden":false,"citation_key":"Davidson:AEPAGT:1993d","source_type":"article","private_publication":false,"abstract":"Backward air mass trajectories for Dye 3, Greenland\n(elevation 2.5 km) show source regions that vary with season: the\ndirection of greatest transport distance is from the southwest in\nfall, west in winter, and northwest in spring; the trajectories in\nsummer do not show a strong preferred direction. Based on 5 d\ntransit times, the trajectories in fall suggest the importance of\nNorth America as a potential source region, with occasional\ntrajectories from western Europe, The trajectories in spring,\nespecially in April, suggest Eurasia (transport over the Pole),\neastern North America, and western Europe as potential source\nregions. Less transport of chemical constituents to Dye 3 is\nexpected in summer when transport distances are shorter. Although\nsome long-range transport to Greenland occurs in winter, the\nstability of the atmosphere over the ice sheet at this time of year\nis likely to limit the delivery of chemical constituents to the\nsurface. Sources outside of these regions can also influence Dye 3\nif transit times longer than 5 d are considered. These results are\nin contrast to trajectories reported by others for sea-level arctic\nlocations such as Barrow, Alaska and Mould Bay, Canada, where\ntransport over the Pole from Eurasia is responsible for high\nchemical species concentrations over much of the winter and early\nspring. Overall, the trajectories are consistent with aerosol\nchemical data for this time period at Dye 3 reported by several\ninvestigators, showing peak concentrations in spring and fall.\nC1 CNRS,GLACIOL & GEOPHYS ENVIRONNEMENT LAB,F-38402 ST MARTIN\nDHERES,FRANCE. ATMOSPHER ENVIRONM SERV,DOWNSVIEW M3H 5T4,ON,CANADA.\nUNIV NEVADA,DESERT RES INST,CTR ATMOSPHER SCI,RENO,NV 89506.","bibtype":"article","author":"Davidson, C I and Jaffrezo, J L and Small, M J and Summers, P W and Olson, M P and Borys, R D","journal":"Atmos Environ Pt A-Gen Top","bibtex":"@article{\n title = {Trajectory analysis of source regions influencing the south greenland ice-sheet during the dye-3 gas and aerosol sampling program},\n type = {article},\n year = {1993},\n pages = {2739-2749},\n volume = {27},\n id = {a3cd914d-57b0-3597-a238-a82659b3bbfb},\n created = {2014-10-08T16:28:18.000Z},\n file_attached = {false},\n profile_id = {363623ef-1990-38f1-b354-f5cdaa6548b2},\n group_id = {02267cec-5558-3876-9cfc-78d056bad5b9},\n last_modified = {2017-03-14T17:32:24.802Z},\n read = {false},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Davidson:AEPAGT:1993d},\n source_type = {article},\n private_publication = {false},\n abstract = {Backward air mass trajectories for Dye 3, Greenland\n(elevation 2.5 km) show source regions that vary with season: the\ndirection of greatest transport distance is from the southwest in\nfall, west in winter, and northwest in spring; the trajectories in\nsummer do not show a strong preferred direction. Based on 5 d\ntransit times, the trajectories in fall suggest the importance of\nNorth America as a potential source region, with occasional\ntrajectories from western Europe, The trajectories in spring,\nespecially in April, suggest Eurasia (transport over the Pole),\neastern North America, and western Europe as potential source\nregions. Less transport of chemical constituents to Dye 3 is\nexpected in summer when transport distances are shorter. Although\nsome long-range transport to Greenland occurs in winter, the\nstability of the atmosphere over the ice sheet at this time of year\nis likely to limit the delivery of chemical constituents to the\nsurface. Sources outside of these regions can also influence Dye 3\nif transit times longer than 5 d are considered. These results are\nin contrast to trajectories reported by others for sea-level arctic\nlocations such as Barrow, Alaska and Mould Bay, Canada, where\ntransport over the Pole from Eurasia is responsible for high\nchemical species concentrations over much of the winter and early\nspring. Overall, the trajectories are consistent with aerosol\nchemical data for this time period at Dye 3 reported by several\ninvestigators, showing peak concentrations in spring and fall.\nC1 CNRS,GLACIOL & GEOPHYS ENVIRONNEMENT LAB,F-38402 ST MARTIN\nDHERES,FRANCE. ATMOSPHER ENVIRONM SERV,DOWNSVIEW M3H 5T4,ON,CANADA.\nUNIV NEVADA,DESERT RES INST,CTR ATMOSPHER SCI,RENO,NV 89506.},\n bibtype = {article},\n author = {Davidson, C I and Jaffrezo, J L and Small, M J and Summers, P W and Olson, M P and Borys, R D},\n journal = {Atmos Environ Pt A-Gen Top}\n}","author_short":["Davidson, C., I.","Jaffrezo, J., L.","Small, M., J.","Summers, P., W.","Olson, M., P.","Borys, R., D."],"bibbaseid":"davidson-jaffrezo-small-summers-olson-borys-trajectoryanalysisofsourceregionsinfluencingthesouthgreenlandicesheetduringthedye3gasandaerosolsamplingprogram-1993","role":"author","urls":{},"downloads":0},"bibtype":"article","biburl":null,"creationDate":"2014-09-11T15:28:59.353Z","downloads":0,"keywords":[],"search_terms":["trajectory","analysis","source","regions","influencing","south","greenland","ice","sheet","during","dye","gas","aerosol","sampling","program","davidson","jaffrezo","small","summers","olson","borys"],"title":"Trajectory analysis of source regions influencing the south greenland ice-sheet during the dye-3 gas and aerosol sampling program","year":1993}