Sentence examples for anomalous circulation from inspiring English sources

A possible explanation may lie in the anomalous circulation on the optic disc in subjects with optic disc drusen [ 14, 19], and in fact the central retinal artery can be bypassed completely [ 19], but this of course is speculation.

Because of these two anomalous circulations, regions from Korea show anomalous to the eastern part of mainland China are under the influence of northeasterly and easterly.

In addition, since there are anomalous southerly between the anomalous cyclonic circulation in the southeast of Japan and the anomalous anticyclonic circulation in the northeast of Japan, TCs in drought years also follow this passage.

Extreme weather events are usually associated with unusual ("anomalous") atmospheric circulation patterns.

Also, the anomalous cyclonic circulation over India is not prominent in the composite (Fig. 6a).

Once developed, however, the temperature anomaly of the ocean surface tends to reinforce and thereby maintain the anomalous atmospheric circulation.

Massom, R. A. et al. Extreme Anomalous Atmospheric Circulation in the West Antarctic Peninsula Region in Austral Spring and Summer 2001/02, and Its Profound Impact on Sea Ice and Biota.

The above analysis shows that the cold waves over India can occur with or without blocking events over the Ural-Siberia region but what is important is the presence of anomalous low temperatures over the Indo-China region which can be advected into the Indian latitudes by the anomalous cyclonic circulation over India.

The western flank of the low level anomalous cyclone over the west coast of India, a response to the Pacific convection anomalies, advects cooler temperatures into northwest India from higher latitudes (Fig. 7f) and the eastern flank of the anomalous cyclonic circulation advects warmer equatorial temperatures into central and northern parts of India (Fig. 7f).

The influence of the anomalous Walker circulation can be seen in the strong anomalous descent near 5°S and moderate descent near 10°N (Fig. 3a, see also Fig. 1a).

Changes in the anomalous secondary circulation, namely anomalous upward (downward) flow in the SWNP and anomalous downward (upward) flow in the mid-latitudes of East Asia, are one of the causes of drought (non-drought).