
Hemispherical transport of volcanic dust inferred from diffuse radiation measurements
Author(s) -
P. S. HARIHARA AYYAR
Publication year - 1966
Publication title -
mausam
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.243
H-Index - 12
ISSN - 0252-9416
DOI - 10.54302/mausam.v17i4.5795
Subject(s) - volcano , southern hemisphere , northern hemisphere , atmospheric sciences , environmental science , geology , vulcanian eruption , climatology , seismology
Volcanic dust has been used in the past as a tracer or' atmospheric motions. The volcanic dust resulting from the eruption of Mt. Agung, Bali (8° S, 115°E) w March 1963 produced some spectacular effects in the southern hemisphere as seen from the radiation observations made at Aspendale (38° S, 145°E). The diffuse radiation mesurements made at Poona, however, do not show such effects to any appreciable extent. It is, therefore, concluded that the transport from the southern to the northern hemisphere of stratospheric dust is of a much smaller magnitude than the transport within the southern hemisphere itself.