In situ observations of ClO in the Arctic stratosphere: ER‐2 aircraft results from 59°N TO 80°N latitude

William Henry Brune, D. W. Toohey, J. G. Anderson, K. R. Chan

Research output: Contribution to journalArticle

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Abstract

Large abundances of ClO were observed inside the arctic polar vortex during 14 flights of the NASA ER‐2 aircraft from Stavanger, Norway (59°N, 6°E) to 80°N latitude. Flights were conducted at altitudes between 14 and 20 km when the solar zenith angle was between 79° and 101°. Data are reported for three flights, January 6, January 16, and Febmary 10, that represent the main features observed during the mission. ClO mixing ratios were typically less than 50 parts per trillion by volume (pptv) outside the vortex and exceeded 100 pptv inside the vortex for all flights. ClO mixing ratios were more than 500 pptv for four days in a row in early February, reaching 1130 pptv on February 10, at an altitude of 19 km (potential temperature of 460 K). Peak ClO mixing ratios in early February were ∼ 100 times larger than those observed at mid‐latitudes for all altitudes surveyed between 15 and 19 km. These data, comparable to those obtained in the antarctic ozone hole, indicate that the springtime arctic polar vortex was extensively perturbed by heterogeneous chemistry and contained enough ClO to catalytically destroy ozone rapidly.

Original languageEnglish (US)
Pages (from-to)505-508
Number of pages4
JournalGeophysical Research Letters
Volume17
Issue number4
DOIs
StatePublished - Jan 1 1990

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stratosphere
aircraft
mixing ratios
flight
mixing ratio
vortices
polar vortex
vortex
ozone
ozone depletion
Norway
temperate regions
zenith angle
zenith
potential temperature
chemistry
in situ
temperature

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Earth and Planetary Sciences(all)

Cite this

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title = "In situ observations of ClO in the Arctic stratosphere: ER‐2 aircraft results from 59°N TO 80°N latitude",
abstract = "Large abundances of ClO were observed inside the arctic polar vortex during 14 flights of the NASA ER‐2 aircraft from Stavanger, Norway (59°N, 6°E) to 80°N latitude. Flights were conducted at altitudes between 14 and 20 km when the solar zenith angle was between 79° and 101°. Data are reported for three flights, January 6, January 16, and Febmary 10, that represent the main features observed during the mission. ClO mixing ratios were typically less than 50 parts per trillion by volume (pptv) outside the vortex and exceeded 100 pptv inside the vortex for all flights. ClO mixing ratios were more than 500 pptv for four days in a row in early February, reaching 1130 pptv on February 10, at an altitude of 19 km (potential temperature of 460 K). Peak ClO mixing ratios in early February were ∼ 100 times larger than those observed at mid‐latitudes for all altitudes surveyed between 15 and 19 km. These data, comparable to those obtained in the antarctic ozone hole, indicate that the springtime arctic polar vortex was extensively perturbed by heterogeneous chemistry and contained enough ClO to catalytically destroy ozone rapidly.",
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In situ observations of ClO in the Arctic stratosphere : ER‐2 aircraft results from 59°N TO 80°N latitude. / Brune, William Henry; Toohey, D. W.; Anderson, J. G.; Chan, K. R.

In: Geophysical Research Letters, Vol. 17, No. 4, 01.01.1990, p. 505-508.

Research output: Contribution to journalArticle

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AB - Large abundances of ClO were observed inside the arctic polar vortex during 14 flights of the NASA ER‐2 aircraft from Stavanger, Norway (59°N, 6°E) to 80°N latitude. Flights were conducted at altitudes between 14 and 20 km when the solar zenith angle was between 79° and 101°. Data are reported for three flights, January 6, January 16, and Febmary 10, that represent the main features observed during the mission. ClO mixing ratios were typically less than 50 parts per trillion by volume (pptv) outside the vortex and exceeded 100 pptv inside the vortex for all flights. ClO mixing ratios were more than 500 pptv for four days in a row in early February, reaching 1130 pptv on February 10, at an altitude of 19 km (potential temperature of 460 K). Peak ClO mixing ratios in early February were ∼ 100 times larger than those observed at mid‐latitudes for all altitudes surveyed between 15 and 19 km. These data, comparable to those obtained in the antarctic ozone hole, indicate that the springtime arctic polar vortex was extensively perturbed by heterogeneous chemistry and contained enough ClO to catalytically destroy ozone rapidly.

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