Intercomparison of total ozone observations at Fairbanks, Alaska, during POLARIS

被引:8
作者
Lloyd, S
Swartz, WH
Kusterer, T
Anderson, D
McElroy, CT
Midwinter, C
Hall, R
Nassim, K
Jaffe, D
Simpson, W
Kelley, J
Nicks, D
Griffin, D
Johnson, B
Evans, R
Quincy, D
Oltmans, S
Newman, P
McPeters, R
Labow, G
Moy, L
Seftor, C
Toon, G
Sen, B
Blavier, JF
机构
[1] Johns Hopkins Univ, Appl Phys Lab, Laurel, MD 20723 USA
[2] Univ Maryland, Dept Chem, College Pk, MD 20742 USA
[3] Environm Canada, Atmospher Environm Serv, Downsview, ON, Canada
[4] Univ Washington, Inst Geophys, Bothell, WA USA
[5] Univ Alaska, Dept Chem, Fairbanks, AK 99775 USA
[6] NOAA, Climate Monitoring & Diagnost Lab, Boulder, CO 80303 USA
[7] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
[8] Raytheon Informat Technol & Sci Serv, Lanham, MD USA
[9] Jet Propuls Lab, Pasadena, CA USA
关键词
D O I
10.1029/1999JD900468
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The pattern of seasonal ozone loss over Fairbanks, Alaska (AK), during the NASA Photochemistry of Ozone Loss in the Arctic Region In Summer (POLARIS) campaign in the spring and summer of 1997 is defined. Five independent data sets of total ozone observations at Fairbanks are presented, from the Earth Probe and ADEOS Total Ozone Mapping Spectrometer (TOMS) satellite instruments, balloon-borne electrochemical concentration cell ozonesondes, and ground-based (Brewer spectroradiometer, Dobson spectrophotometer, and the Jet Propulsion Laboratory MkIV infrared interferometer) instruments. The excellent agreement between different observational techniques lends confidence to the observed rate of summertime loss of total ozone at high latitudes. In addition, the small offsets between the data sets are well understood.
引用
收藏
页码:26767 / 26778
页数:12
相关论文
共 14 条
[1]   An assessment of ECC ozonesondes operated using 1% and 0.5% KI cathode solutions at Lauder, New Zealand [J].
Boyd, IS ;
Bodeker, GE ;
Connor, BJ ;
Swart, DPJ ;
Brinksma, EJ .
GEOPHYSICAL RESEARCH LETTERS, 1998, 25 (13) :2409-2412
[2]  
Dobson G.M.B., 1929, P ROY SOC LOND, VA122, P456, DOI DOI 10.1098/RSPA.1929.0034
[3]   Ozone, column ClO, and PSC measurements made at the NDSC Eureka observatory (80 degrees N, 86 degrees W) during the spring of 1997 [J].
Donovan, DP ;
Fast, H ;
Makino, Y ;
Bird, JC ;
Carswell, AI ;
Davies, J ;
Duck, TJ ;
Kaminski, JW ;
McElroy, CT ;
Mittermeier, RL ;
Pal, SR ;
Savastiouk, V ;
Velkov, D ;
Whiteway, JA .
GEOPHYSICAL RESEARCH LETTERS, 1997, 24 (22) :2709-2712
[4]   An assessment of the world ground-based total ozone network performance from the comparison with satellite data [J].
Fioletov, VE ;
Kerr, JB ;
Hare, EW ;
Labow, GJ ;
McPeters, RD .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1999, 104 (D1) :1737-1747
[5]   Long-term ozone decline over the Canadian Arctic to early 1997 from ground-based and balloon observations [J].
Fioletov, VE ;
Kerr, JB ;
Wardle, DI ;
Davies, J ;
Hare, EW ;
McElroy, CT ;
Tarasick, DW .
GEOPHYSICAL RESEARCH LETTERS, 1997, 24 (22) :2705-2708
[6]  
GAINES S, 1998, PHOTOCHEMISTRY OZONE
[7]  
KERR JB, 1984, P QUADR INT OZ S HAL, P381
[8]  
KERR JB, 1984, P QUADR OZ S HALD GR, P396
[9]  
KOMHYR WD, 1969, ANN GEOPHYS, V25, P203
[10]   An assessment of the accuracy of 14.5 years of Nimbus 7 TOMS Version 7 ozone data by comparison with the Dobson network [J].
McPeters, RD ;
Labow, GJ .
GEOPHYSICAL RESEARCH LETTERS, 1996, 23 (25) :3695-3698