Immediate and accurate detection of airborne volcanic ash is an operational
imperative of the aviation industry, especially jet aircraft. Ash encounte
rs place passengers aboard these aircraft at severe risk and significantly
impact, via forced rerouting, both the safety and profit margins of freight
carriers due to their limited fuel supply. Moreover the airlines can suffe
r high economic costs for repair and -replacement of equipment. Operational
detection. and tracking of volcanic ash by most national weather services
has relied heavily on a split window differencing technique of thermal long
wave infrared channels on currently operational satellites. Unfortunately,
prior work on volcanic ash defection has not emphasised the dynamical inter
action between the erupting volcano and the effects of overlying atmospheri
c Lr;ater vapor phreatic and phreatomagmatic water sources. Six volcanic as
h eruptions from around the globe were chosen for study because they have w
ide variation in ambient atmospheric water vapor, available ground and surf
ace water and different magma types. Results show that the present differen
cing technique is not uniformly effective in properly classifying volcanic
ash pixels in the satellite scene and often falsely interprets meteorologic
al clouds as volcanic ash clouds and conversely. Moreover it is not always
a robust early detector, an operational aviation requirement. Seasonal vari
ability in global integrated atmospheric water vapor coupled with the geogr
aphical distribution of currently active volcanoes, suggests the concerns d
iscussed herein with regard to six specific eruptions, have applicability t
o the global aviation industry. Operational implications are discussed and
a strategic proposal is presented on necessary steps to improve detection.
(C) Elsevier Science Inc., 2000.