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Page 1: RAMMB: Regional and Mesoscale Meteorology Branchrammb.cira.colostate.edu/resources/docs/31May96.pdf · was the surface warm front. Consider the NMC3 surface analyses for 0900, 1200,
Page 2: RAMMB: Regional and Mesoscale Meteorology Branchrammb.cira.colostate.edu/resources/docs/31May96.pdf · was the surface warm front. Consider the NMC3 surface analyses for 0900, 1200,
Page 3: RAMMB: Regional and Mesoscale Meteorology Branchrammb.cira.colostate.edu/resources/docs/31May96.pdf · was the surface warm front. Consider the NMC3 surface analyses for 0900, 1200,
Page 4: RAMMB: Regional and Mesoscale Meteorology Branchrammb.cira.colostate.edu/resources/docs/31May96.pdf · was the surface warm front. Consider the NMC3 surface analyses for 0900, 1200,
Page 5: RAMMB: Regional and Mesoscale Meteorology Branchrammb.cira.colostate.edu/resources/docs/31May96.pdf · was the surface warm front. Consider the NMC3 surface analyses for 0900, 1200,
Page 6: RAMMB: Regional and Mesoscale Meteorology Branchrammb.cira.colostate.edu/resources/docs/31May96.pdf · was the surface warm front. Consider the NMC3 surface analyses for 0900, 1200,
Page 7: RAMMB: Regional and Mesoscale Meteorology Branchrammb.cira.colostate.edu/resources/docs/31May96.pdf · was the surface warm front. Consider the NMC3 surface analyses for 0900, 1200,
Page 8: RAMMB: Regional and Mesoscale Meteorology Branchrammb.cira.colostate.edu/resources/docs/31May96.pdf · was the surface warm front. Consider the NMC3 surface analyses for 0900, 1200,
Page 9: RAMMB: Regional and Mesoscale Meteorology Branchrammb.cira.colostate.edu/resources/docs/31May96.pdf · was the surface warm front. Consider the NMC3 surface analyses for 0900, 1200,
Page 10: RAMMB: Regional and Mesoscale Meteorology Branchrammb.cira.colostate.edu/resources/docs/31May96.pdf · was the surface warm front. Consider the NMC3 surface analyses for 0900, 1200,
Page 11: RAMMB: Regional and Mesoscale Meteorology Branchrammb.cira.colostate.edu/resources/docs/31May96.pdf · was the surface warm front. Consider the NMC3 surface analyses for 0900, 1200,
Page 12: RAMMB: Regional and Mesoscale Meteorology Branchrammb.cira.colostate.edu/resources/docs/31May96.pdf · was the surface warm front. Consider the NMC3 surface analyses for 0900, 1200,
Page 13: RAMMB: Regional and Mesoscale Meteorology Branchrammb.cira.colostate.edu/resources/docs/31May96.pdf · was the surface warm front. Consider the NMC3 surface analyses for 0900, 1200,
Page 14: RAMMB: Regional and Mesoscale Meteorology Branchrammb.cira.colostate.edu/resources/docs/31May96.pdf · was the surface warm front. Consider the NMC3 surface analyses for 0900, 1200,
Page 15: RAMMB: Regional and Mesoscale Meteorology Branchrammb.cira.colostate.edu/resources/docs/31May96.pdf · was the surface warm front. Consider the NMC3 surface analyses for 0900, 1200,
Page 16: RAMMB: Regional and Mesoscale Meteorology Branchrammb.cira.colostate.edu/resources/docs/31May96.pdf · was the surface warm front. Consider the NMC3 surface analyses for 0900, 1200,
Page 17: RAMMB: Regional and Mesoscale Meteorology Branchrammb.cira.colostate.edu/resources/docs/31May96.pdf · was the surface warm front. Consider the NMC3 surface analyses for 0900, 1200,