@Book{793154669,
author="Kaifler, Bernd",
title="Thermal structure and gravity waves in the Antarctic middle atmosphere observed by lidar",
year="2013",
abstract="The IAP iron Doppler lidar has been operated at the Antarctic station Davis (69{\textdegree}S, 78{\textdegree}E) between December 2010 and December 2012. Seasonal variations in the thermal structure above Davis are studied and wave-induced temperature perturbations are analyzed on different time scales. Gravity wave potential energy densities (GWPED) are computed from stratospheric and mesospheric lidar observations and compared to a simple gravity wave model. It is shown that observed seasonal variations in GWPED are caused by selective filtering of zonally propagating gravity waves.",
note="vorgelegt von: Bernd Kaifler",
note="Rostock, Univ., Mathematisch-Naturwiss. Fak., Diss., 2014",
url="http://rosdok.uni-rostock.de/resolve?urn=urn:nbn:de:gbv:28-diss2014-0104-4",
url="http://rosdok.uni-rostock.de/resolve?urn=urn:nbn:de:gbv:28-diss2014-0104-4&pdf",
url="http://nbn-resolving.de/urn:nbn:de:gbv:28-diss2014-0104-4",
language="English"
}