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During the Canadian Atlantic Storms Program (CASP) field project from 15 January to 15 March 1986, seven storms underwent rapid deepening either within or adjacent to the observational network. The most rapid deepening phase of these storms was associated with the surface low-pressure centre being located close to to the rain-snow boundary ami the end of this phase was associated with the low centre eventually moving to sub-freezing surface temperatures. Precipitation bat& of both rain and snowdoi:10.1080/07055900.1989.9649329 fatcat:mds2xcfgb5fr7bxwarlegeim2u