Quantifying transport between the tropical and mid-latitude lower stratosphere

被引:139
作者
Volk, CM
Elkins, JW
Fahey, DW
Salawitch, RJ
Dutton, GS
Gilligan, JM
Proffitt, MH
Loewenstein, M
Podolske, JR
Minschwaner, K
Margitan, JJ
Chan, KR
机构
[1] UNIV COLORADO,COOPERAT INST RES ENVIRONM SCI,BOULDER,CO 80309
[2] NOAA,AERON LAB,BOULDER,CO 80303
[3] CALTECH,JET PROP LAB,PASADENA,CA 91109
[4] NASA,AMES RES CTR,MOFFETT FIELD,CA 94035
[5] NEW MEXICO INST MIN & TECHNOL,DEPT PHYS,SOCORRO,NM 87801
关键词
D O I
10.1126/science.272.5269.1763
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Airborne in situ observations of molecules with a wide range of lifetimes (methane, nitrous oxide, reactive nitrogen, ozone, chlorinated halocarbons, and halon-1211), used in a tropical tracer model, show that mid-latitude air is entrained into the tropical lower stratosphere within about 13.5 months; transport is faster in the reverse direction, Because exchange with the tropics is slower than global photochemical models generally assume, ozone at mid-latitudes appears to be more sensitive to elevated levels of industrial chlorine than is currently predicted, Nevertheless, about 45 percent of air in the tropical ascent region at 21 kilometers is of mid-latitude origin, implying that emissions from supersonic aircraft could reach the middle stratosphere.
引用
收藏
页码:1763 / 1768
页数:6
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