NLCs at Svalbard by lidar

In summer 2001 a potassium lidar was installed near Longyearbyen (78 • N) on the north polar island of Spitsbergen which is part of the archipelago Svalbard. At the same place a series of meteorological rockets (" falling spheres " , FS) were launched which gave temperatures from the lower thermosphere to the stratosphere. The potassium 5 lidar is capable of detecting noctilucent clouds (NLCs) and of measuring temperatures in the lower thermosphere, both under daylight conditions. In this paper we give an overview on the NLC measurements (the first at this latitude) and compare the results with temperatures from meteorological rockets which have been published recently (L ¨ ubken and M ¨ ullemann, 2003). NLCs were observed from 12 June (the first day 10 of operation) until 12 August when a period of bad weather started. When the lidar was switched on again on 26 August, no NLC was observed. The mean occurrence frequency in the period 12 June – 12 August (" lidar NLC period ") is 77%. The mean of all individual NLC peak altitudes is 83.6 km (variability: 1.1 km). The mean peak NLC altitude does not show a significant variation with season. The average top and bottom 15 altitude of the NLC layer is 85.1 and 82.5 km, respectively, with a variability of ∼1.2 km. The mean of the maximum volume backscatter coefficient β max at our wavelength of 770 nm is 3.9×10 −10 /m/sr with a large variability of ±3.8×10 −10 /m/sr. Comparison of NLC characteristics with measurements at ALOMAR (69 • N) shows that the peak altitude and the maximum volume backscatter coefficient are similar at both locations 20 but NLCs occur more frequently at higher latitudes. Simultaneous temperature and NLC measurements are available for 3 flights and show that the NLC layer occurs in the lower part of the height range with super-saturation. The NLC peak occurs over a large range of degree of saturation (S) whereas most models predict the peak at S=1. This demonstrates that steady-state 25 considerations may not be applicable when relating individual NLC properties to background conditions. On the other hand, the mean variation of the NLC appearance with height and season is in agreement with the climatological variation of super-saturation 522 Abstract Introduction Conclusions References Tables Figures Back Close Full Screen / Esc Print Version Interactive Discussion c EGU 2003 derived from the FS temperature measurements.