Editorial Type:
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Article Type:
Research Article

Snowbands during the Cold-Air Outbreak of 23 January 2003

David M. Schultz Cooperative Institute for Mesoscale Meteorological Studies, University of Oklahoma, and NOAA/National Severe Storms Laboratory, Norman, Oklahoma

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Derek S. Arndt Oklahoma Climatological Survey, University of Oklahoma, Norman, Oklahoma

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David J. Stensrud NOAA/National Severe Storms Laboratory, Norman, Oklahoma

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Jay W. Hanna NOAA/NESDIS Satellite Services Division, Camp Springs, Maryland

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Print Publication:
01 Mar 2004
Collections:
Pictures of the Month in Monthly Weather Review
DOI:
https://doi.org/10.1175/1520-0493(2004)132<0827:SDTCOO>2.0.CO;2
Page(s):
827–842
Restricted access

Abstract

A cold-air outbreak east of the Rocky Mountains on 23 January 2003 produced banded clouds and snow across the central and southeastern United States. The bands occurred through two processes: 1) thermal instability in the planetary boundary layer produced horizontal convective rolls (HCRs) over widespread areas, and 2) lake-effect processes downstream of small lakes (fetch < 100 km) produced localized bands. Characteristics of the observed bands associated with the HCRs, such as horizontal scale, depth of circulation, orientation, duration, and dynamics, are explored through observations, previous literature, and theoretical models. Snow from clouds produced by HCRs over land during the cold season has not been extensively studied previously. In this event, cold-air advection over the warm ground led to an upward sensible heat flux, promoting the occurrence of the HCR circulations. As the surface temperature decreased, the height of the lifting condensation level decreased, eventually forming cloud bands within the ascending portion of the HCR circulations. Ice crystals are inferred to have fallen from a large-scale precipitation system aloft into the cloud bands in the planetary boundary layer, which was within the favored temperature regime for dendritic growth of ice crystals. The ice crystals grew and reached the surface as light snow. This seeder–feeder process suggests one way to anticipate development of such snowbands in the future, as demonstrated by other similar events on other days in Oklahoma and Illinois. As the cloud bands were advected equatorward, they ingested drier air and dissipated. Among the several lake-effect bands observed on 23 January 2003, one notable band occurred downwind of Lake Kentucky. Midlake convergence of the land breeze may have initially produced a narrow cloud band that broadened as the land breeze ended. That the snowbands due to the HCRs and lake effect were both associated with heat and/or moisture fluxes from the earth's surface highlights the potential importance of ground- and water-surface temperature measurements for accurate numerical weather prediction.

Corresponding author address: Dr. David M. Schultz, NOAA/NSSL, 1313 Halley Circle, Norman, OK 73069. Email: david.schultz@noaa.gov

Abstract

A cold-air outbreak east of the Rocky Mountains on 23 January 2003 produced banded clouds and snow across the central and southeastern United States. The bands occurred through two processes: 1) thermal instability in the planetary boundary layer produced horizontal convective rolls (HCRs) over widespread areas, and 2) lake-effect processes downstream of small lakes (fetch < 100 km) produced localized bands. Characteristics of the observed bands associated with the HCRs, such as horizontal scale, depth of circulation, orientation, duration, and dynamics, are explored through observations, previous literature, and theoretical models. Snow from clouds produced by HCRs over land during the cold season has not been extensively studied previously. In this event, cold-air advection over the warm ground led to an upward sensible heat flux, promoting the occurrence of the HCR circulations. As the surface temperature decreased, the height of the lifting condensation level decreased, eventually forming cloud bands within the ascending portion of the HCR circulations. Ice crystals are inferred to have fallen from a large-scale precipitation system aloft into the cloud bands in the planetary boundary layer, which was within the favored temperature regime for dendritic growth of ice crystals. The ice crystals grew and reached the surface as light snow. This seeder–feeder process suggests one way to anticipate development of such snowbands in the future, as demonstrated by other similar events on other days in Oklahoma and Illinois. As the cloud bands were advected equatorward, they ingested drier air and dissipated. Among the several lake-effect bands observed on 23 January 2003, one notable band occurred downwind of Lake Kentucky. Midlake convergence of the land breeze may have initially produced a narrow cloud band that broadened as the land breeze ended. That the snowbands due to the HCRs and lake effect were both associated with heat and/or moisture fluxes from the earth's surface highlights the potential importance of ground- and water-surface temperature measurements for accurate numerical weather prediction.

Corresponding author address: Dr. David M. Schultz, NOAA/NSSL, 1313 Halley Circle, Norman, OK 73069. Email: david.schultz@noaa.gov

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  • Agee, E. M., 1976: Observational evidence of cell flatness as a function of convective depth and cell anisotropy. J. Meteor. Soc. Japan, 54 , 68–71.

    • Search Google Scholar
    • Export Citation

  • Asai, T., 1970: Stability of a plane parallel flow with variable vertical shear and unstable stratification. J. Meteor. Soc. Japan, 48 , 129–139.

    • Search Google Scholar
    • Export Citation

  • Atkinson, B. W., and J. W. Zhang, 1996: Mesoscale shallow convection in the atmosphere. Rev. Geophys., 34 , 403–431.

  • Atlas, D., S-H. Chou, and W. P. Byerly, 1983: The influence of coastal shape on winter mesoscale air–sea interaction. Mon. Wea. Rev., 111 , 245–252.

    • Search Google Scholar
    • Export Citation

  • Brock, F. V., K. C. Crawford, R. L. Elliott, G. W. Cuperus, S. J. Stadler, H. L. Johnson, and M. D. Eilts, 1995: The Oklahoma Mesonet: A technical overview. J. Atmos. Oceanic Technol., 12 , 5–19.

    • Search Google Scholar
    • Export Citation

  • Brown, R. A., 1980: Longitudinal instabilities and secondary flows in the planetary boundary layer: A review. Rev. Geophys. Space Phys., 18 , 683–697.

    • Search Google Scholar
    • Export Citation

  • Cairns, M. M., R. Collins, T. Cylke, M. Deutschendorf, and D. Mercer, 2001a: A lake effect snowfall in western Nevada—Part I: Synoptic setting and observations. Preprints, 18th Conf. on Weather Analysis and Forecasting, Fort Lauderdale, FL, Amer. Meteor. Soc., 329–332.

    • Search Google Scholar
    • Export Citation

  • Cairns, M. M., J. Corey, and D. R. Koracin, 2001b: A numerical simulation of a rare lake-effect snowfall in western Nevada. Preprints, 18th Conf. on Weather Analysis and Forecasting, Fort Lauderdale, FL, Amer. Meteor. Soc., J62–J64.

    • Search Google Scholar
    • Export Citation

  • Carpenter, D. M., 1993: The lake effect of the Great Salt Lake: Overview and forecast problems. Wea. Forecasting, 8 , 181–193.

  • Chang, H-R., and H. N. Shirer, 1984: Transitions in shallow convection: An explanation for lateral cell expansion. J. Atmos. Sci., 41 , 2334–2346.

    • Search Google Scholar
    • Export Citation

  • Clark, T. L., T. Hauf, and J. P. Kuettner, 1986: Convectively forced internal gravity waves: Results from two-dimensional numerical experiments. Quart. J. Roy. Meteor. Soc., 112 , 899–925.

    • Search Google Scholar
    • Export Citation

  • Cotton, W. R., and R. A. Anthes, 1989: Storm and Cloud Dynamics. Academic Press, 883 pp.

  • Fukuta, N., and T. Takahashi, 1999: The growth of atmospheric ice crystals: A summary of findings in vertical supercooled cloud tunnel studies. J. Atmos. Sci., 56 , 1963–1979.

    • Search Google Scholar
    • Export Citation

  • Grossman, R. L., 1982: An analysis of vertical velocity spectra obtained in the BOMEX fair-weather, trade-wind boundary layer. Bound.-Layer Meteor., 23 , 323–357.

    • Search Google Scholar
    • Export Citation

  • Helfand, H. M., and E. Kalnay, 1983: A model to determine open or closed cellular convection. J. Atmos. Sci., 40 , 631–650.

  • Hjelmfelt, M. R., and R. R. Braham Jr., 1983: Numerical simulation of the airflow over Lake Michigan for a major lake-effect snow event. Mon. Wea. Rev., 111 , 205–219.

    • Search Google Scholar
    • Export Citation

  • Holroyd, E. W., 1971: Lake-effect cloud bands seen from weather satellites. J. Atmos. Sci., 28 , 1165–1170.

  • Huggins, A. W., D. E. Kingsmill, and M. M. Cairns, 2001: A lake effect snowfall in western Nevada—Part II: Radar characteristics and quantitative precipitation estimates. Preprints, 18th Conf. on Weather Analysis and Forecasting, Fort Lauderdale, FL, Amer. Meteor. Soc., 333–337.

    • Search Google Scholar
    • Export Citation

  • Kain, J. S., P. R. Janish, S. J. Weiss, M. E. Baldwin, R. S. Schneider, and H. E. Brooks, 2003: Collaboration between forecasters and research scientists at the NSSL and SPC: The Spring Program. Bull. Amer. Meteor. Soc., 84 , 1797–1806.

    • Search Google Scholar
    • Export Citation

  • Kalnay, E., and Coauthors, 1996: The NCEP/NCAR 40-Year Reanalysis Project. Bull. Amer. Meteor. Soc., 77 , 437–471.

  • Kelly, R. D., 1982: A single Doppler radar study of horizontal-roll convection in a lake-effect snow storm. J. Atmos. Sci., 39 , 1521–1531.

    • Search Google Scholar
    • Export Citation

  • Kelly, R. D., 1984: Horizontal roll and boundary-layer interrelationships observed over Lake Michigan. J. Atmos. Sci., 41 , 1816–1826.

  • Krishnamurti, R., 1975: On cellular cloud patterns. Part 1: Mathematical model. J. Atmos. Sci., 32 , 1353–1363.

  • Kristovich, D. A. R., 1993: Mean circulations of boundary-layer rolls in lake-effect snow storms. Bound.-Layer Meteor., 63 , 293–315.

  • Kuettner, J., 1937: Die atmosphärischen Gleichgewichts-Verhältnisse über Lappland im Polarsommer. Beitr. Phys. Atmos., 24 , 98–114.

  • Kuettner, J., 1959: The band structure of the atmosphere. Tellus, 11 , 267–294.

  • Kuettner, J., 1971: Cloud bands in the earth's atmosphere: Observations and theory. Tellus, 23 , 404–425.

  • Kuettner, J., P. A. Hildebrand, and T. L. Clark, 1987: Convection waves: Observations of gravity wave systems over convectively active boundary layers. Quart. J. Roy. Meteor. Soc., 113 , 445–467.

    • Search Google Scholar
    • Export Citation

  • Kuo, H. L., 1963: Perturbations of plane Couette flow in stratified fluid and origin of cloud streets. Phys. Fluids, 6 , 195–211.

  • LeMone, M. A., and R. J. Meitín, 1984: Three examples of fair-weather mesoscale boundary-layer convection in the Tropics. Mon. Wea. Rev., 112 , 1985–1997.

    • Search Google Scholar
    • Export Citation

  • Ligda, M. G. H., and S. G. Bigler, 1958: Radar echoes from a cloudless cold front. J. Meteor., 15 , 494–501.

  • Maletzke, R., 1953: Die meteorologischen Vorbedingungen des 1000 km Segelflugs. Schweiz. Aero Rev., 28 , 191–192.

  • Miura, Y., 1986: Aspect ratios of longitudinal rolls and convection cells observed during cold air outbreaks. J. Atmos. Sci., 43 , 29–39.

    • Search Google Scholar
    • Export Citation

  • Niziol, T. A., 1987: Operational forecasting of lake effect snowfall in western and central New York. Wea. Forecasting, 2 , 310–321.

  • Niziol, T. A., W. R. Snyder, and J. S. Waldstreicher, 1995: Winter weather forecasting throughout the eastern United States. Part IV: Lake effect snow. Wea. Forecasting, 10 , 61–77.

    • Search Google Scholar
    • Export Citation

  • Onton, D. J., and W. J. Steenburgh, 2001: Multiscale analysis of the 7 December 1998 Great Salt Lake–effect snowstorm. Mon. Wea. Rev., 129 , 1318–1338.

    • Search Google Scholar
    • Export Citation

  • Passarelli Jr., R. E., and R. R. Braham Jr., 1981: The role of the winter land breeze in the formation of Great Lake snow storms. Bull. Amer. Meteor. Soc., 62 , 482–491.

    • Search Google Scholar
    • Export Citation

  • Peace, R. L., and R. B. Sykes Jr., 1966: Mesoscale study of a lake-effect snowstorm. Mon. Wea. Rev., 94 , 495–507.

  • Powers, J. G., and M. T. Stoelinga, 2000: A coupled air–sea mesoscale model: Experiments in atmospheric sensitivity to marine roughness. Mon. Wea. Rev., 128 , 208–228.

    • Search Google Scholar
    • Export Citation

  • Sasaki, Y., 1970: Influences of thermal boundary layer on atmospheric cellular convection. J. Meteor. Soc. Japan, 48 , 492–502.

  • Schultz, D. M., and P. N. Schumacher, 1999: The use and misuse of conditional symmetric instability. Mon. Wea. Rev., 127 , 2709–2732. Corrigendum, 128, 1573.

    • Search Google Scholar
    • Export Citation

  • Schultz, D. M., W. E. Bracken, L. F. Bosart, G. J. Hakim, M. A. Bedrick, M. J. Dickinson, and K. R. Tyle, 1997: The 1993 Superstorm cold surge: Frontal structure, gap flow, and tropical impact. Mon. Wea. Rev., 125 , 5–39. Corrigendum, 125, 662.

    • Search Google Scholar
    • Export Citation

  • Schultz, D. M., W. E. Bracken, and L. F. Bosart, 1998: Planetary- and synoptic-scale signals associated with Central American cold surges. Mon. Wea. Rev., 126 , 5–27.

    • Search Google Scholar
    • Export Citation

  • Shafer, M. A., C. A. Fiebrich, D. Arndt, S. E. Fredrickson, and T. W. Hughes, 2000: Quality assurance procedures in the Oklahoma Mesonetwork. J. Atmos. Oceanic Technol., 17 , 474–494.

    • Search Google Scholar
    • Export Citation

  • Shirer, H. N., 1986: On cloud street development in three dimensions: Parallel and Rayleigh instabilities. Contrib. Atmos. Phys., 59 , 126–149.

    • Search Google Scholar
    • Export Citation

  • Shirer, H. N., and B. Brümmer, 1986: Cloud streets during KonTur: A comparison of parallel/thermal instability modes with observations. Contrib. Atmos. Phys., 59 , 150–161.

    • Search Google Scholar
    • Export Citation

  • Steenburgh, W. J., and D. J. Onton, 2001: Multiscale analysis of the 7 December 1998 Great Salt Lake–effect snowstorm. Mon. Wea. Rev., 129 , 1296–1317.

    • Search Google Scholar
    • Export Citation

  • Steenburgh, W. J., S. F. Halvorson, and D. J. Onton, 2000: Climatology of lake-effect snowstorms of the Great Salt Lake. Mon. Wea. Rev., 128 , 709–727.

    • Search Google Scholar
    • Export Citation

  • Walter, B. A., 1980: Wintertime observations of roll clouds over the Bering Sea. Mon. Wea. Rev., 108 , 2024–2031.

  • Weckwerth, T. M., J. W. Wilson, R. M. Wakimoto, and N. A. Crook, 1997: Horizontal convective rolls: Determining the environmental conditions supporting their existence and characteristics. Mon. Wea. Rev., 125 , 505–526.

    • Search Google Scholar
    • Export Citation

  • Weckwerth, T. M., T. W. Horst, and J. W. Wilson, 1999: An observational study of the evolution of horizontal convective rolls. Mon. Wea. Rev., 127 , 2160–2179.

    • Search Google Scholar
    • Export Citation

  • Wilken, G. R., 1997: A lake-effect snow in Arkansas. NWS Southern Region Tech. Attachment SR/SSD 97-21, 5 pp. [Available online at http://www.srh.noaa.gov/ftproot/topics/attach/html/ssd97-21.htm.].

    • Search Google Scholar
    • Export Citation

  • Wilson, J. W., T. M. Weckwerth, J. Vivekanandan, R. M. Wakimoto, and R. W. Russell, 1994: Boundary-layer clear-air radar echoes: Origins of echoes and accuracy of derived winds. J. Atmos. Oceanic Technol., 11 , 1184–1206.

    • Search Google Scholar
    • Export Citation

  • Young, G. S., D. A. R. Kristovich, M. R. Hjelmfelt, and R. C. Foster, 2002: Rolls, streets, waves, and more: A review of quasi-two-dimensional structures in the atmospheric boundary layer. Bull. Amer. Meteor. Soc., 83 , 997–1001. ES54–ES69.

    • Search Google Scholar
    • Export Citation
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