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Aircraft observations of NO, NO y , CO, and O 3 in the upper troposphere from 60°N to 60°S ‐ Interhemispheric differences at mitlatitudes
Measurements of NO, NO y , CO, and O 3 made in the middle and upper troposphere over Punta Arenas, Chile (53°S) and Prestwick, Scotland (55°N) during the INCA (Interhemispheric Differences in Cirrus Properties from Anthropogenic Emissions) experiment in 2000 are used to examine the interhemispheric...
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Published in: | Geophysical research letters 2003-06, Vol.30 (11) |
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container_title | Geophysical research letters |
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creator | Baehr, Janine Schlager, Hans Ziereis, Helmut Stock, Paul van Velthoven, Peter Busen, Reinhold Ström, Johan Schumann, Ulrich |
description | Measurements of NO, NO
y
, CO, and O
3
made in the middle and upper troposphere over Punta Arenas, Chile (53°S) and Prestwick, Scotland (55°N) during the INCA (Interhemispheric Differences in Cirrus Properties from Anthropogenic Emissions) experiment in 2000 are used to examine the interhemispheric differences in the abundance of these species during local autumn. Median mixing ratios of NO, NO
y
, O
3
, and CO in the upper troposphere (8 km‐tropopause) are 4.5, 3, 1.5 and 1.2 times higher over Prestwick compared to Punta Arenas, respectively. Corresponding enhancement factors for the middle troposphere are 5, 7.8, 1.5, and 1.4. The present data represent a considerable extension of the sparse NO and NO
y
data so far available for the middle and upper troposphere at southern midlatitudes. |
doi_str_mv | 10.1029/2003GL016935 |
format | article |
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y
, CO, and O
3
made in the middle and upper troposphere over Punta Arenas, Chile (53°S) and Prestwick, Scotland (55°N) during the INCA (Interhemispheric Differences in Cirrus Properties from Anthropogenic Emissions) experiment in 2000 are used to examine the interhemispheric differences in the abundance of these species during local autumn. Median mixing ratios of NO, NO
y
, O
3
, and CO in the upper troposphere (8 km‐tropopause) are 4.5, 3, 1.5 and 1.2 times higher over Prestwick compared to Punta Arenas, respectively. Corresponding enhancement factors for the middle troposphere are 5, 7.8, 1.5, and 1.4. The present data represent a considerable extension of the sparse NO and NO
y
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y
, CO, and O
3
made in the middle and upper troposphere over Punta Arenas, Chile (53°S) and Prestwick, Scotland (55°N) during the INCA (Interhemispheric Differences in Cirrus Properties from Anthropogenic Emissions) experiment in 2000 are used to examine the interhemispheric differences in the abundance of these species during local autumn. Median mixing ratios of NO, NO
y
, O
3
, and CO in the upper troposphere (8 km‐tropopause) are 4.5, 3, 1.5 and 1.2 times higher over Prestwick compared to Punta Arenas, respectively. Corresponding enhancement factors for the middle troposphere are 5, 7.8, 1.5, and 1.4. The present data represent a considerable extension of the sparse NO and NO
y
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y
, CO, and O
3
made in the middle and upper troposphere over Punta Arenas, Chile (53°S) and Prestwick, Scotland (55°N) during the INCA (Interhemispheric Differences in Cirrus Properties from Anthropogenic Emissions) experiment in 2000 are used to examine the interhemispheric differences in the abundance of these species during local autumn. Median mixing ratios of NO, NO
y
, O
3
, and CO in the upper troposphere (8 km‐tropopause) are 4.5, 3, 1.5 and 1.2 times higher over Prestwick compared to Punta Arenas, respectively. Corresponding enhancement factors for the middle troposphere are 5, 7.8, 1.5, and 1.4. The present data represent a considerable extension of the sparse NO and NO
y
data so far available for the middle and upper troposphere at southern midlatitudes.</abstract><doi>10.1029/2003GL016935</doi></addata></record> |
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language | eng |
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source | Wiley-Blackwell AGU Digital Archive |
title | Aircraft observations of NO, NO y , CO, and O 3 in the upper troposphere from 60°N to 60°S ‐ Interhemispheric differences at mitlatitudes |
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