首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >TROPOSPHERIC OZONE DURING MAUNA LOA OBSERVATORY PHOTOCHEMISTRY EXPERIMENT 2 COMPARED TO LONG-TERM MEASUREMENTS FROM SURFACE AND OZONESONDE OBSERVATIONS
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TROPOSPHERIC OZONE DURING MAUNA LOA OBSERVATORY PHOTOCHEMISTRY EXPERIMENT 2 COMPARED TO LONG-TERM MEASUREMENTS FROM SURFACE AND OZONESONDE OBSERVATIONS

机译:相较于从表面和臭氧探空仪进行的长期测量,莫纳河口观测光学化学实验2中的对流臭氧

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摘要

Continuous surface ozone measurements have been made at Mama Loa Observatory (MLO) for 20 years. In addition, weekly ozone profile measurements using balloonborne ozonesondes have been carried out from Hilo, Hawaii, since 1985. These long-term records are compared with data obtained during the MLOPEX 2 period from September 1991 to August 1992. Ozone behavior at the observatory level (similar to 3.4 km) during autumn and winter of 1991-1992 was similar to that found during the period 1980-1990. In spring and summer 1992, however, there were several significant differences from the long-term behavior. During March and April 1992, there was about 10% more ozone than the long-term average, and the variability was less than half of what is seen normally. These characteristics are associated with strong flow from the north and west. Both June and July 1992 saw periods of elevated ozone with the June average 20% higher than normal. During the more limited sampling (weekly profiles) when ozonesonde measurements were made, the 1992 spring enhancement was particularly pronounced at 500 mbar (similar to 6 km), while during the summer the larger than normal concentrations were at 700 mbar (similar to 3.5 km). In the upper troposphere, on the other hand, spring ozone amounts in 1992 were much below normal with only about half the ozone usually seen in the 12- to 15-km region. The ozone profiles are discussed in terms of the representativeness of the MLO surface measurements in characterizing the free troposphere ozone behavior at both the altitude of the observatory as well as other heights in the atmosphere. During the winter and spring, the MLO measurements are often representative of behavior over a broad depth of the troposphere (3-10 km). In the summer and autumn the MLO observations are more characteristic of free tropospheric conditions at or near the observatory level. [References: 14]
机译:妈妈罗阿天文台(MLO)连续进行了20年的臭氧表面测量。此外,自1985年以来,从夏威夷的希洛开始使用气球式臭氧探空仪进行每周臭氧剖面测量。将这些长期记录与1991年9月至1992年8月的MLOPEX 2时期获得的数据进行了比较。 1991-1992年秋冬季期间的(大约3.4 km)与1980-1990年期间的相似。但是,在1992年春季和夏季,与长期行为存在一些显着差异。在1992年3月和4月期间,臭氧比长期平均水平多出约10%,而变异性还不到正常值的一半。这些特征与来自北部和西部的强劲水流有关。 1992年6月和7月都出现臭氧升高的时期,6月的平均水平比正常高20%。在进行臭氧探空仪测量的更有限的采样期间(每周概况),1992年春季的增强在500 mbar(约6 km)时尤为明显,而在夏季,浓度高于正常值的700 mbar(约3.5 km)明显高于正常水平)。另一方面,在对流层上方,1992年春季的臭氧量大大低于正常水平,通常在12至15公里区域仅见到一半的臭氧。臭氧分布图是根据MLO表面测量的代表性来讨论的,以表征天文台高度以及大气中其他高度的自由对流层臭氧行为。在冬季和春季,MLO测量值通常代表对流层较宽深度(3-10 km)内的行为。在夏季和秋季,MLO的观测更具有天文台水平或附近的对流层自由状态的特征。 [参考:14]

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