caa a22 4500 469084405 CHVBK 20180323133000.0 cr unu---uuuuu 170328e19920901xx s 000 0 eng 10.1007/BF02656940 doi (NATIONALLICENCE)springer-10.1007/BF02656940 McHall Y. Dept. of Meteorology, University of Edinburgh, EH9 3JZ, UK aut Wintertime stratospheric anomalies— Part I: Warm pools [Elektronische Daten] [Y. McHall] The stratospheric worm pools, called the 4-day wave also, are mainly the temperature anomalies in the polar regions of winter hemisphere. It will be shown that their occurrence, propagation speed and specific structure can be explained by the lower frequency coherent heating resulting from the wave interaction in the breaking layers of the stratosphere. Although their vertical phase slope is negligibly small, the warm pools cannot be considered as a barotropic anomaly. Advances in Atmospheric Sciences, 1992 Advances in Atmospheric Sciences Springer-Verlag 9/3(1992-09-01), 299-310 0256-1530 9:3<299 1992 9 376 https://doi.org/10.1007/BF02656940 text/html Onlinezugriff via DOI 1 research-article jats NATIONALLICENCE 856 40 https://doi.org/10.1007/BF02656940 text/html Onlinezugriff via DOI NATIONALLICENCE 100 1- McHall Y. Dept. of Meteorology, University of Edinburgh, EH9 3JZ, UK aut NATIONALLICENCE 773 0- Advances in Atmospheric Sciences Springer-Verlag 9/3(1992-09-01), 299-310 0256-1530 9:3<299 1992 9 376 Metadata rights reserved Springer special CC-BY-NC licence nationallicence BK010053 XK010053 XK010000 NATIONALLICENCE NATIONALLICENCE NL-springer