Charged particle measurements in the polar summer mesosphere obtained by the DROPPS sounding rockets

Abstract Two Black Brant V sounding rocket payloads (DROPPS) were flown as part of the DROPPS/MIDAS program from the Andoya Rocket Range, Norway, during July 1999. One of these payloads was launched during the presence of PMSE, and the other flight occurred during NLC conditions. Both payloads were equipped to measure a number of different electrodynamic parameters of the mesosphere and lower thermosphere. A fixed-bias Langmuir probe observed small-scale structure in electron concentration. Significant electron depletions (more than an order of magnitude) were measured in a narrow altitude region during both flights. Layers of a thickness between 300 and 1400 meters were observed with very sharp transitions at the edges of the layers. These electron depletions do not appear to be artifacts produced by electrode collisions with large positive particulates. Absolute electron density concentrations were determined by a multiple-frequency radio wave propagation experiment. In addition, ion conductivities, mobilities, and number densities were determined by a Gerdien condenser. In this paper, we report on the instrumentation and the preliminary observations of the charged particle environment.

[1]  E. Kopp,et al.  Small‐scale structure of O2+ and proton hydrates in a noctilucent cloud and polar mesospheric summer echo of August 9/10 1991 above Kiruna , 1993 .

[2]  John Y. N. Cho,et al.  A comparison of PMSE and other ground-based observations during the NLC-91 campaign , 1995 .

[3]  Robert H. Holzworth,et al.  The DROPPS program to study the polar summer mesosphere , 2001 .

[4]  G. Witt,et al.  Positive ion depletion in a noctilucent cloud , 1996 .

[5]  J. Röttger,et al.  First observations of summer polar mesospheric backscatter with a 224 MHz radar , 1988 .

[6]  H. Rishbeth,et al.  Simultaneous observations of noctilucent clouds and polar mesospheric radar echoes: Evidence of non-correlation , 1989 .

[7]  J. Bremer,et al.  Simultaneous and common‐volume observations of noctilucent clouds and polar mesosphere summer echoes , 1999 .

[8]  J. Röttger,et al.  Polar mesosphere summer echoes observed with the EISCAT 933-MHz radar and the CUPRI 46.9-MHz radar, their similarity to 224-MHz radar echoes and their relation to turbulence and electron density profiles , 1989 .

[9]  W. Ecklund,et al.  Comparison of simultaneous MST radar and electron density probe measurements during STATE , 1988 .

[10]  W. Muir Earthquake-Proof Buildings , 1885, Nature.

[11]  J. Hall,et al.  D-REGION ELECTRON DENSITIES AND COLLISION FREQUENCIES FROM FARADAY ROTATION AND DIFFERENTIAL ABSORPTION MEASUREMENTS. , 1972 .

[12]  J. Röttger,et al.  The structure and dynamics of polar mesosphere summer echoes observed with the EISCAT 224 MHz radar , 1988 .

[13]  W. Ecklund,et al.  Long‐term observations of the Arctic mesosphere with the MST radar at Poker Flat, Alaska , 1981 .

[14]  John Y. N. Cho,et al.  An updated review of polar mesosphere summer echoes: Observation, theory, and their relationship to noctilucent clouds and subvisible aerosols , 1997 .