Extreme winds at northern mid-latitudes since 1871

Summertime ozone at northern mid-latitudes

Evidence linking Arctic amplification to extreme weather in mid-latitudes

[1] Arctic amplification (AA) – the observed enhanced warming in high northern latitudes relative to the northern hemisphere – is evident in lower-tropospheric temperatures and in 1000-to-500 hPa thicknesses. Daily fields of 500 hPa heights from the National Centers for Environmental Prediction Reanalysis are analyzed over N. America and the N. Atlantic to assess changes in north-south (Rossby)...

Convective gravity waves at mid-latitudes

Wind-profiler observations of gravity waves produced by convection at mid-latitudes Y. G. Choi, S. C. Lee, A. J. McDonald, and D. A. Hooper Geophysical Prospecting Laboratory, Seoul National University, Korea Department of Physics, Kangnung National University, Korea Department of Physics and Astronomy, University of Canterbury, Private Bag 4800, Christchurch, New Zealand Rutherford Appleton La...

Cirrus, contrails, and ice supersaturated regions in high pressure systems at northern mid latitudes

During the European heat wave summer 2003 with predominant high pressure conditions we performed a detailed study of upper tropospheric humidity and ice particles which yielded striking results concerning the occurrence of ice supersaturated regions (ISSR), cirrus, and contrails. Our study is based on lidar observations and meteorological data obtained at Lindenberg/Germany (52.2 N, 14.1 E) as ...

Carnivores in Northern Latitudes

The first mammals were probably nocturnal (McNab 1978; Kemp 1982) and many extant orders of small mammals have retained this trait. This behaviour is presumably due to the measure of protection from predation that darkness provides (Crawford 1934; Falls 1968; Daan and Aschoff 1982). Large, herbivorous mammals are less restricted to the nocturnal phase (e.g. Bunnell and Harestad 1990) and have b...