Zobrazeno 1 - 10
of 79
pro vyhledávání: '"A. L. SCHMELTEKOPF"'
Autor:
Thomas L. Thompson, R. Wilson, R. H. Winkler, A. L. Schmeltekopf, R. J. McLaughlin, Adrian F. Tuck, K. K. Kelly, Erik Richard
Publikováno v:
Applied Physics B: Lasers and Optics. 75:183-194
We describe a near-infrared in situ tunable diode laser spectrometer developed for atmospheric measurements of CH4 in the upper troposphere and lower stratosphere (UT/LS). The instrument is designed to provide fast-response (0.5–1 Hz) measurements
Publikováno v:
Journal of Mass Spectrometry. 32:1273-1278
Publikováno v:
Geophysical Research Letters. 21:2535-2538
The Stratospheric Photochemistry, Aerosols, and Dynamics Expedition (SPADE) made in situ observations of the composition of the lower stratosphere from the NASA ER-2 aircraft at latitudes from 15°N to 60°N, during November 1992 and April, May and O
Autor:
J. P. Smith, J. G. Keys, A. L. Schmeltekopf, Sean C. Solomon, L. Perliski, H. L. Miller, R. W. Sanders
Publikováno v:
Journal of Geophysical Research: Atmospheres. 98:8983-8989
Ground-based measurements of NO3 absorption in the band near 662 nm were carried out on four occasions using the Moon as a light source during sunrise at both middle and polar latitudes. As the Sun rose, the observed slant column abundance of atmosph
Autor:
J. P. Smith, S. Solomon, J. G. Keys, L. Perliski, George H. Mount, A. L. Schmeltekopf, R. W. Sanders, H. L. Miller
Publikováno v:
Journal of Geophysical Research: Atmospheres. 98:7219-7228
This paper presents results from a series of measurements of atmospheric OClO covering the period April to October 1991, made at McMurdo Station, Antarctica. These measurements were made to extend the knowledge of the general role of atmospheric chlo
Autor:
J. G. Keys, H. L. Miller, L. Perliski, S. Solomon, J. P. Smith, R. W. Sanders, George H. Mount, A. L. Schmeltekopf
Publikováno v:
Journal of Geophysical Research: Atmospheres. 98:993-1000
Lunar absorption spectra have been used to determine the vertical column abundances of NO[sub 2] and NO[sub 3] above McMurdo Station, Antarctica (77.8[degrees]S), during the fall, winter, and spring seasons in 1991. The observed nighttime NO[sub 2] a
Autor:
E. E. Ferguson, Fred C. Fehsenfeld, M. McFarland, D. L. Albritton, Werner Lindinger, A. L. Schmeltekopf
Publikováno v:
The Journal of Chemical Physics. 63:2175-2181
The forward and reverse rate constants for the proton‐transfer reaction, N2OH++CO?COH++N2O, have been measured as a function of temperature in a variable‐temperature flowing afterglow and as a function of relative kinetic energy in a flow‐drift
Autor:
H. I. Schiff, A. L. Schmeltekopf, Carleton J. Howard, J. R. McAfee, J. A. Davidson, G. E. Streit
Publikováno v:
The Journal of Chemical Physics. 67:5021-5025
Absolute rate constants are reported for the deactivation of O(1D) by five trace atmospheric constituents for the temperature range 200–350 K. O(1D) atoms produced by photolyzing ozone with a frequency quadrupled pulse from a Nd‐YAG laser are mon
Publikováno v:
The Journal of Chemical Physics. 65:4761-4764
Absolute rate constants and their temperature dependencies for the deactivation of O(1D) by five important atmospheric gases are reported. O(1D) atoms are produced by photolysis of ozone at 266 nm and the atoms are directly observed in time resolved
Autor:
Dieter Kley, K. K. Kelly, R. H. Winkler, M. McFarland, Thomas L. Thompson, A. L. Schmeltekopf
Publikováno v:
Geophysical Research Letters. 9:617-620
Total water was measured in the high troposphere and low stratosphere over Panama during ten aircraft flights. The results show that convective storms provide the means of transporting water into the stratosphere. From a consideration of the anvil he