Summary
Joining together or merging is postulated to be a major way in which convective clouds become larger, enhancing their transports and impacts upon their environment. Cumulus shower merger is defined in terms of echoes from a calibrated digitized 10-cm radar reviewing a 0.9×105 km2 area in south Florida, U. S. A., which encompasses a 1.3×104 km2 experimental area for randomized seeding.
A detailed physical and statistical study is reported for three relatively undisturbed untreated days in the summer of 1973, the driest of which was a randomly selected control day for the experiment. Mergers are found to produce more than an order of magnitude more rain than unmerged echoes, while mergers of mergers (second order mergers) produce still an order of magnitude more rain. On the three days studied, merged systems produced about 86% of the rainfall over the area. Duration, echo area and rain depths are also compared for merged and unmerged systems. Each day is then analyzed individually, indicating a correlation between organization and rain amount, confirmed by other research reviewed briefly.
The location and time of merger is related to the seabreeze convergence zones as predicted by the University of Virginia Mesoscale Model with overall good agreement. Physical hypotheses suggesting the importance of downdrafts in cumulus merging are developed. The relevance of mergers to hydrology, weather modification and the large-scale impacts of convective clouds is discussed.
Zusammenfassung
Das Zusammenwachsen oder Verschmelzen von Cumulus-Wolken wird als einer der Hauptgründe für ihr Wachstum sowie für ihren Einfluß auf ihre Umgebung und auf die durch sie bewerkstelligten Transportprozesse angesehen. Das Verschmelzen von Cumulus-Schauern wird auf Grund der von einem kalibrierten und digitisierten 10-cm-Radar empfangenen Echos definiert. Das Radargerät überblickt eine Fläche von 0.9×105 km2 im Süden Floridas (U. S. A.), die ein Exerimentalgebiet von 1.3×104 km2 für randomisierte Wolkenimpfung umgibt.
Eine detaillierte physikalische und statistische Studie für drei relativ ungestörte Tage ohne Wolkenimpfung während des Sommers 1973 wird hiermit vorgelegt. Der trockenste dieser Tage war willkürlich als Kontrolltag für das Wolkenimpfungsexperiment gewählt worden. Verschmelzungsprozesse weisen um mehr als eine Größenordnung mehr Niederschlag auf als unverschmolzene Echos, während Verschmelzungen von Verschmelzungen (Verschmelzungen zweiter Ordnung) nochmals eine Größenordnung mehr Regen ergeben. An den drei untersuchten Tagen produzierten verschmolzene Systeme ungefähr 86% des über dem Untersuchungsgebiet beobachteten Regens. Andauer, Echoausmaß und Niederschlagshöhe werden für verschmolzene und unverschmolzene Wolkensysteme verglichen. Jeder Tag wird individuell analysiert, wobei eine Korrelation zwischen Wolkenorganisation und Niederschlagsbetrag angedeutet wird, die auch von anderen, kurz erwähnten Forschungsarbeiten bekräftigt wurde.
Ort und Zeit des Verschmelzens hängen von der Seewind-Konvergenzzone ab, welche durch das mesoskalare Rechenmodell der University of Virginia gut vorhergesagt wurde. Eine physikalische Hypothese über die Wichtigkeit der Absinkbewegung während des Cumulus-Verschmelzungsprozesses wird dargelegt. Die Bedeutung der Verschmelzungsvorgänge für die Hydrologie, für die künstliche Wetterbeeinflussung und für den großräumigen Einfluß konvektiver Wolken wird diskutiert.
Similar content being viewed by others
References
Austin, P. M., Mason, C. K., Kraus, M. J.: Mesoscale Precipitation Patterns in New England and Their Relation to Macroscale Parameters. 12th Conf. on Radar Met., pp. 234–240, Norman, Oklahoma (1966).
Battan, L. J.: Duration of Convective Radar Cloud Units. Bull. Amer. Met. Soc.32, 227–228 (1953).
Betts, A. K.: A Composite Mesoscale Cumulonimbus Budget. J. Atmos. Sci.30, 597–610 (1973).
Betts, A. K.: Convection in the Tropics. Meteorology Over the Tropical Oceans. Roy Met. Soc., pp. 105–132, Bracknell, England (1978).
Bjerknes, J.: Saturated Adiabatic Ascent of Air Through Dry Adiabatically Descending Environment. Quart. J. R. Met. Soc.64, 325–330 (1938).
Browing, K. A.: The Structure and Mechanisms of Hailstorms. Hail: A Review of Hail Science and Hail Suppression. Met. Monographs16, No. 38. Amer. Met Soc., pp. 1–43, Boston, Mass. (1977).
Byers, H. R., Braham, R. R., Jr.: The Thunderstorm: Report of the Thunderstorm Project, 287 pp. Washington, D. C.: U. S. Government Printing Office 1949.
Chen, C.-H., Orville, H. D.: Effects of Mesoscale Convergence on Cloud Convection. Submitted to J. Appl. Met. (1979).
Cotton, W. R.: Theoretical Cumulus Dynamics. Rev. Geophys.13, 419–448 (1975).
Cotton, W. R., Pielke, R. A.: Weather Modification and Three-Dimensional Mesoscale Models. Bull. Amer. Met. Soc.57, 788–796 (1976).
Cotton, W. R., Pielke, R. A., Gannon, P. T.: Numerical Experiments on the Influence of the Mesoscale Circulation on the Cumulus Scale. J. Atmos. Sci.33, 252–261 (1976).
Cotton, W. R., Tripoli, G. J.: Effects of Mesoscale Convergence on Three-Dimensional Simulations of Large Cumulus Clouds. Submitted to J. Atmos. Sci. (1979).
Cressman, G. P.: The Influence of the Field of Horizontal Divergence on Convective Cloudiness. J. Met.3, 85–88 (1946).
Cunning, J., Thomas, J., Gannon, P.: Mesoscale Response of the Florida Environment to Convection-a Case Study. Preprint Vol. Tenth Conf. on Severe Local Storms, Amer. Met. Soc., pp. 126–132, Omaha, Nebraska (1977).
Eden, J. C.: Guide to Computer Programs Used in the Statistical Analysis of Florida Cumulus Seeding Experiments. NOAA Tech. Memorandum ERL WMPO-14, 117 pp., Boulder, Colorado (1974).
Frank, H., Lhermitte, R. M.: Cell Interaction and Merger in a South Florida Thunderstorm. 17th Conf. Radar Meteor. Amer. Soc., pp. 151–156, Seattle, Washington (1976).
Frank, N. L., Moore, P. L., Fisher, G. E.: Summer Shower Distribution Over the Florida Peninsula as Deduced From Digitized Radar Data. J. Appl. Met.6, 309–316 (1967).
Fritsch, J. M.: Cumulus Dynamics: Local Compensating Subsidence and Its Implications for Cumulus Parameterization. Pageoph.113, 851–867 (1975).
Fritsch, J. M., Chappell, C. F.: Numerical Prediction of Convectively Driven Mesoscale Pressure Systems. Preprint Vol. Fourth Conf. on Weather Forecasting and Analysis and Aviation Meteorology, Amer. Met. Soc., pp. 77–87 (1978).
Gannon, P. T.: Influence of Earth Surface and Cloud Properties on the South Florida Seabreeze. NOAA Tech. Report ERL 402 NHEML 2, 91 pp., U. S. Dept. of Commerce, Boulder, Colorado (1978).
Gerrish, R., Hiser, H. W.: Mesoscale Studies of Instability Patterns and Winds in the Tropics. Rept. 7, 63 pp. U. S. Army Elec. Labs., Fort Monmouth, New Jersey (1965).
Herndon, A., Woodley, W. L., Miller, A. H., Samet, A., Sern, H.: Comparison of Gage and Radar Methods of Convective Precipitation Measurement, NOAA Tech. Memo. ERL OD-18, Boulder, Colorado (1973).
Hill, G. E.: Factors Controlling the Size and Spacing of Cumulus Clouds as Revealed by Numerical Experiments. J. Atmos. Sci.31, 646–673 (1974).
Holle, R. L., Cunning, J., Thomas, J., Gannon, P., Teijeiro, L.: A Case Study of Mesoscale Convection and Cloud Merger Over South Florida. 11th Tech. Conf. on Hurricanes and Tropical Meteorology, Miami Beach, Florida, Amer. Met. Soc., pp. 428–4235 (1977).
Holle, R. L., Maier, M. W.: Cloud Interaction and the Formation of the 15 June 1973 Tornado in the FACE Mesonetwork. NOAA Tech. Memo. ERL-WMPO33, 55 pp. (1976).
Leary, C. A., Houze, R. A., Jr.: The Structure and Evolution of Convection in a Tropical Cloud Cluster. J. Atmos. Sci.36, 437–457 (1979).
Lilly, D. K.: Dynamical Structure and Evolution of Thunderstorms and Squall Lines. Ann. Rev. Earth Planet Sci.7, 117–161 (1979).
Ludlam, F. H., Scorer, R. S.: Reviews of Modern Meteorology 10: Convection in the Atmosphere. Quart. J. R. Met. Soc.79, 317–341 (1953).
Mahrer, Y., Pielke, R. A.: The Effects of Topography on Sea and Land Breezes in Two-Dimensional Numerical Model. Mon. Weath. Rev.105, 1151–1162 (1977).
Mahrer, Y., Pielke, R. A.: A Test of an Upstream Spline Interpolation Technique for the Advective Terms in a Numerical Mesoscale Model. Mon. Weath. Rev.106, 818–830 (1978).
Malkus, J. S.: Effects of Wind Shear on Some Aspects of Convection. Trans. Amer. Geophys. Union30, 19–25 (1949).
Malkus, J. S.: Recent Advances in the Study of Convective Clouds and Their Interaction With the Environment. Tellus4, 71–87 (1952).
Malkus, J. S.: The Slopes of Cumulus Clouds in Relation to External Wind Shear. Quart. J. R. Met. Soc.78, 530–542 (1952).
Malkus, J. S.: Some Results of a Trade Cumulus Clouds Investigation. J. Met.11, 220–237 (1954).
Malkus, J. S.: On the Formation and Structure of Downdrafts in Cumulus Clouds. J. Met.12, 350–357 (1955).
Malkus, J. S., Riehl, H.: Cloud Structure and Distributions Over the Tropical Pacific Ocean, 229 pp. Univ. of California Press, Berkeley (1964).
Malkus, J. S., Scorer, R. S.: The Erosion of Cumulus Towers. J. Met.12, 43–57 (1955).
Malkus, J. S., Williams, R. T.: On the Interaction Between Severe Storms and Large Cumulus Clouds. Met. Monographs5, 59–64 (1963).
Moncrieff, M. W., Miller, M. J.: The Dynamics and Simulation of Tropical Cumulonimbus and Squall Lines. Quart. J. R. Met. Soc.102, 373–394 (1976).
National Center for Atmospheric Research: Report of the U. S. GATE Central Program Workshop, 723 pp. Ed. R. Greenfield (1977).
Pielke, R.: A Three-Dimensional Numerical Model of the Sea Breezes Over South Florida. Mon. Weath. Rev.102, 115–139 (1974).
Pielke, R. A., Cotton, W. R.: A Mesoscale Analysis Over South Florida for a High Rainfall Event. Mon. Weath. Rev.105, 343–362 (1977).
Pielke, R. A., Cotton, W. R.: The Evolutionary Characteristics of Sea and Lake-Breeze Generated Convective-Mesoscale Systems Over South Florida. Submitted to Mon. Weath. Rev. (1979).
Pielke, R. A., Mahrer, Y.: The Numerical Simulation of the Airflow Over Barbados. Mon. Weath. Rev.104, 1392–1402 (1976).
Pielke, R. A., Mahrer, Y.: A Numerical Study of the Airflow Over Irregular Terrain. Beitr. Physik Atmos.50, 98–113 (1977).
Pielke, R. A., Mahrer, Y.: Verification Analysis of the University of Virginia Mesoscale Model Prediction Over South Florida for 1 July 1973. Mon. Weath. Rev.106, 1568–1589 (1978).
Plank, V. G.: The Size of Cumulus Clouds in Representative Florida Populations. J. Appl. Met.8, 46–67 (1969).
Saunders, P. M.: An Observational Study of Cumulus. J. Met.18, 451–467 (1961).
Schlesinger, R. E.: A Three-Dimensional Numerical Model of an Isolated Thunderstorm. Part I. Comparative Experiments for Variable Ambient Wind Shear. J. Atmos. Sci.35, 690–713 (1978).
Scorer, R. S., Ludlam, F. H.: Bubble Theory of Penetrative Convection. Quart. J. R. Met. Soc.79, 94–103 (1953).
Simpson, J.: Downdrafts as Linkages in Dynamic Cumulus Seeding Effects. Submitted to J. Appl. Met. (1979).
Simpson, J., Dennis, A. S.: Cumulus Clouds and Their Modification. Weather Modification, Chap. 6, pp. 229–280 (Hess, W. N., ed.). New York: Wiley 1974.
Simpson, J., Woodley, W. L.: Seeding Cumulus in Florida — New 1970 Results. Science172, 117–126 (1971).
Simpson, J., Woodley, W. L.: Florida Area Cumulus Experiment 1970–1973 Rainfall Results. J. Appl. Met.14, 734–744 (1975).
Sims, A. L., Mueller, E. A., Stout, G. E.: Investigations of Quantitative Determination of Point and Areal Precipitation by Radar Echo Measurements. Quart. Tech. Rep., 1 July 63-30 Sept. 1963, 27 pp., Met. Lab., Illinois State Water Survey, Urbana (1963).
Snedecor, G. W., Cochran, W. G.: Statistical Methods. The Iowa State University Press, Ames, Iowa (1967).
Staff, Experimental Meteorology Laboratory: 1973 Florida Area Cumulus Experiment (FACE) Operational and Preliminary Summary. NOAA Techn. Memo. ERL WMPO-12, 254 pp., Boulder, Colorado (1974).
Thomas, J., Jordan, J.: Measurement of Convective Rainfall Within the FACE Target Area. Abstract Vol. 7th Conf. on Weather Modification, Amer. Met. Soc., Banff, Alberta, Canada (1979).
Ulanski, S., Garstang, M.: The Role of Surface Divergence and Vorticity in the Life Cycle of Convective Rainfall. Part I: Observation and Analysis. J. Atmos. Sci.35, 1047–1062 (1978).
Ulanski, S., Garstang, M.: The Role of Surface Divergence and Vorticity in the Life Cycle of Convective Rainfall. Part II; Descriptive Model. J. Atmos. Sci.35, 1063–1069 (1978).
Ulanski, S., Garstang, M.: Some Aspects of Florida Convective Rainfall. Water Resources Research14, 1133–1139 (1978).
Warner, C., Simpson, J., Van Helvoirt, G.: Shallow and Deep Convection: Day 261 of GATE. Tech. Report No. 4, Cloud Populations and Their Interactions With the Boundary Layer. Dept. of Environmental Sciences, 90 pp. University of Virginia, Charlottesville, Virginia.
Welch, B. L.: The Significance of the Difference Between Two Means When the Population Variance Are Unequal. Biometrika (Cambridge, England)29, 350–359 (1938).
Westcott, N. E.: Radar Characterization of South Florida Convective Rainfall. Proc. Sixth Conf. on Planned and Inadvertent Weather Modification, pp. 190–193. Champaign-Urbana, Illinois. Amer. Met. Soc. (1977).
Westcott, N. E.: Radar Characterization of South Florida Rainfall, 74 pp. M. S. Thesis, Dept. of Environmental Sciences, University of Virginia, Charlottesville, Virginia (1977).
Westcott, N. E., Simpson, J.: Population Study of Radar Echoes Over South Florida. Submitted to J. Appl. Met. (1979).
Wiggert, V., Andrews, G. F.: Digitizing, Recording, and Computer Processing Weather Data at EML. NOAA Tech. Memo. ERL WMPO-17, pp. 1–25 (1974).
Wiggert, V., Lockett, G. J., Ostlund, S.: Radar Rainshower Growth Histories and Their Variation With Wind Speed and Echo Motion Over South Florida. Submitted to Mon. Weath. Rev. (1979).
Wiggert, V., Ostlund, S.: Computerized Rain Assessment and Tracking of South Florida WSR-57 Weather Radar Echoes. Bull. Amer. Met. Soc.56, 17–26 (1975).
Wiggert, V., Ostlund, S., Lockett, G. J., Stewart, J. V.: Computer Software for the Assessment of Growth Histories of Weather Radar Echoes. NOAA Tech. Mem. ERL WMPO-35, 85 pp. Boulder, Colorado (1976).
Wilson, J. W.: Evaluation of Precipitation Measurements With the WSR-57 Weather Radar. J. Appl. Met.3, 164–174 (1964).
Woodley, W. L., Jordan, J. A., Simpson, J., Biondini, R., Flueck, J.: NOAA's Florida Area Cumulus Experiment Rainfall Results: 1970–1976. In press.
Woodley, W. L., Norwood, J., Sancho, B.: Some Aspects of South Florida Showers and Thunderstorms. Weatherwise24, 106–113 (1971).
Woodley, W. L., Olsen, A., Herndon, A., Wiggert, V.: Optimizing the Measurement of Convective Rainfall in Florida. NOAA Tech. Mem. ERL WMPO-18, 99 pp. Boulder, Colorado (1974).
Woodley, W. L., Olsen, A. R., Herndon, A., Wiggert, V.: Comparison of Gage and Radar Methods of Convective Rain Measurement. J. Appl. Met.14, 909–928 (1975).
Woodley, W. L., Sax, R. I.: The Florida Area Cumulus Experiment: Rationale, Design, Procedures, Results and Future Course. NOAA Tech. Rept. ERL 354-WMPO 6, 204 pp. (1976).
Woodley, W. L., Simpson, J., Biondini, R., Berkeley, J.: Rainfall Results, 1970–1975: Florida Area Cumulus Experiment. Science195, 735–742.
Woodley, W. L., Simpson, J., Biondini, R., Jordan, J.: NOAA's Florida Area Cumulus Experiment Rainfall Results 1970–1976. Sixth Conf. on Inadvertent and Planned Weather Modification, pp. 206–209. Champaign-Urbana, Illinois, Amer. Met. Soc. (1977).
Author information
Authors and Affiliations
Additional information
With 11 Figures
Rights and permissions
About this article
Cite this article
Simpson, J., Westcott, N.E., Clerman, R.J. et al. On cumulus mergers. Arch. Met. Geoph. Biokl. A. 29, 1–40 (1980). https://doi.org/10.1007/BF02247731
Received:
Issue Date:
DOI: https://doi.org/10.1007/BF02247731