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ToolsRaizada, Shikha, Rapp, Markus, Labken, F.-J., Haffner, J., Zecha, M. and Plane, J. M. C. (2007) Effect of ice particles on the mesospheric potassium layer at Spitsbergen (78°N). Journal of Geophysical Research D: Atmospheres, 112 (8).
Full text not available from this repository.Abstract
This paper quantitatively evaluates the influence of ice particles on the K layer by using radar and lidar measurements. The methodology involves determination of the volumetric surface area [Aice] of the ice particles in a noctilucent cloud by combining a microphysical ice particle model with a charging model to produce an empirical proxy for polar mesosphere summer echoes (PMSE) based on the properties of the charged aerosol particles. The altitudinal variation of [Aice] reveals peak values of about 2.2 × 10−8 cm−1 around 85 km. The first-order loss rate of atomic K due to uptake on the ice particles maximizes close to 2.2 × 10−4 s−1 at 85 km. To examine the variability of [Aice] on background parameters, a sensitivity study showed that a ±10% variation in [Aice] can result from either a ±5 K shift in the temperatures relative to a background profile or from a ±30% change in the water vapor concentration. We found that the peak [Aice] remains constant for a change of +4 to –6 K temperature fluctuations over the altitude range of 83–85 km. Finally, a new atmospheric model of potassium predicts profiles of the K layer in early May and July that are in good agreement with the observations, when the seasonally averaged K ablation flux at 79°N is set to 160 atom cm−2 s−1. This study reveals that both the vertical wind and ice particles play a significant role in controlling the K layer distribution at high latitudes.
| Item Type: | Article |
|---|---|
| Faculty \ School: | Faculty of Science > School of Environmental Sciences |
| Depositing User: | Rosie Cullington |
| Date Deposited: | 27 Feb 2011 11:21 |
| Last Modified: | 24 Sep 2024 09:43 |
| URI: | https://ueaeprints.uea.ac.uk/id/eprint/25147 |
| DOI: | 10.1029/2005JD006938 |
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