Abstract
The winter orographic storms over the San Juan Mountains and the Sierra Nevada are compared. The topography of the San Juans is complex while the Sierra barrier is comparatively simple. The barrier jet is well developed upwind of the Sierra Nevada and its development is restricted upwind of the San Juans. The major difference between the storms on the two barriers is that the Sierra Nevada storms are typically maritime while the San Juan storms are continental. The implications for seeding are discussed.
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References
Cooper, W. A., and J. D. Marwitz, 1980: Winter storms over the San Juan Mountains. Part III: Seeding potential. J. Appl. Meteor., 19, 942–949.
Cooper, W. A., and C. P. R. Saunders, 1980: Winter storms over the San Juan Mountains. Part II: Microphysical processes. J. Appl. Meteor., 19, 927–941.
Hallett, J., and S. Mossop, 1974: Production of secondary ice particles during the riming process. Nature, 249, 26–28.
Hobbs, P. V., L. F. Radke, J. R. Fleming and D. G. Atkinson, 1975: Airborne ice nucleus and cloud microstructure measurements in natural and artificially seeded situations over the San Juan Mountains of Colorado. Research Report X, Contributions from the Cloud Physics Group, University of Washington, 89 pp.
Marwitz, J. D., 1974: An airflow case study over the San Juan Mountains of Colorado. J. Appl. Meteor., 13, 450–458.
Marwitz, J. D., 1980: Winter storms over the San Juan Mountains. Part I: Dynamical processes. J. Appl. Meteor., 19, 913–926.
Marwitz, J. D., 1983: The kinematics of orographic airflow during Sierra storms. J. Atmos. Sci., 40, 1218–1227.
Marwitz, J. D., 1987a: Wintertime orographic storms over the Sierra. Part I: Ther- modynamic and kinematic structure. J. Atmos. Sci. (in press).
Marwitz, J. D., 1987b: Wintertime orographic storms over the Sierra. Part II: The precipitation process. J. Atmos. Sci. (in press).
Marwitz, J. D., W. A. Cooper and C. P. R. Saunders, 1976: Structure and seed-ability of San Juan storms. Report No. AS 118, Dept. of Atmospheric Science, University of Wyoming, 329 pp.
Mossop, S., 1976: Production of secondary ice particles during the growth of graupel by riming. Quart. J. Roy. Meteor. Soc., 102, 45–57.
Mossop, S., 1978: The influence of drop size distribution on the production of secondary ice crystals during graupel growth. Quart. J. Roy. Meteor. Soc., 104, 323–330.
Parish, T., 1982: Barrier winds along the Sierra Nevada Mountains. J. Appl. Meteor., 21, 925–930.
Pruppacher, H., and J. Klett, 1980: Microphysics of Clouds and Precipitation D. Reidel, 714 pp.
Waight, K., 1984: A numerical study of the Sierra barrier jet. M.S. thesis, Dept. of Atmospheric Science, University of Wyoming, 119 pp.
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© 1986 American Meteorological Society
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Marwitz, J. (1986). A Comparison of Winter Orographic Storms over the San Juan Mountains and the Sierra Nevada. In: Precipitation Enhancement—A Scientific Challenge. Meteorological Monographs. American Meteorological Society, Boston, MA. https://doi.org/10.1007/978-1-935704-17-1_11
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DOI: https://doi.org/10.1007/978-1-935704-17-1_11
Publisher Name: American Meteorological Society, Boston, MA
Online ISBN: 978-1-935704-17-1
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