Incorporation of time continuity into subsynoptic analysis by using dynamical constraints
By: John M. Lewis and Stephen C. Bloom
References
-
Achtemeir
, G. L. 1975. An objective streamline analysis. Unpublished manuscript. Illinois State Water Survey, Champaign, Illinois. -
Bergthorsson
, P.and Döds, B. 1955. Numerical weather map analysis. Tellus, 329– 340. -
Cressman
, G. P. 1959. An operational objective analysis system. Mon. Wea. Rev. 87, 367– 374. -
Cressman
, G. P. 1960. Improved terrain effects in baro-tropic forecasts. Mon. Wea. Rev. 88, 327– 342. -
Eisen
, P. A. 1972. A mesoscale study of the Oklahoma squall line of 8 and 9 June 1966. M.S. Thesis, Penn. State Univ., Dept. of Meteor. -
Fankhauser
, J. C. 1974. The derivation of consistent fields of wind and geopotential height from meso-scale rawinsonde data. J. Appl. Meteor. 13, 637– 646. -
Hill
, K.and Turner, R. E. 1977. NASA's Atmospheric Variability Experiments (AVE). Bull. Amer. Meteor. Soc. 58, 170– 172. -
Hovermale
, J. B.and Cahir, J. J. 1974. Studies of subsynoptic scale circulation associated with jet streaks. Dept. of Meteor., Penn. State Uni v. 125 pp. -
Inman
, R. L. 1970. Papers on operational objective analysis schemes at the National Severe Storms Fore-cast Center. NOAA ERLTM-NSSL. 91 pp. -
Lettau
, H. H. 1959. Wind profile, surface stress and geo-strophic drag coefficients in the atmospheric surface layers . In: Advances in geophysics, Vol. 6. New York: Pergamon Press, pp. 241– 257. -
Lewis
, J. M. 1975. Test of the Ogura-Cho model on a prefrontal squall line case. Mon. Wea. Rev. 103, 764– 778. -
Lewis
, J. M.and Grayson, T. H. 1972. The adjustment of surface wind and pressure by Sasaki's variational matching technique. J. Appl. Meteor. 11, 586– 597. -
Lewis
, J. M., Ogura, Y.and Gidel, L. 1974. Large-scale influences upon the generation of a mesoscale distur-bance. Mon. Wea. Rev. 102, 545– 560. -
Miller
, R. C. 1967. Notes on the analysis and severe-storm forecasting procedures of the military weather warning center. U.S. Air Weather Service Tech. Rept. No. 200, Kansas City, Mo. -
Newman
, W. R. 1972. The relationship between horizon-tal moisture convergence and severe storm occur-rences. M.S. Thesis, Univ. of Okla. -
Ogura
, Y.and Chen, Y. L. 1977. A life history of an intense mesoscale convective storm in Oklahoma. J. Atmos. Sci. 34, 1458– 1476. -
Oleyar
, J. E. 1972. An investigation of the mechanisms of squall line formation. M.S. Thesis, Penn. State Univ., Dept. of Meteor. -
Sangster
, W. E. 1960. A method of representing the horizontal pressure force without reduction of station pressures to sea level. J. Meteor. 17, 166– 176. -
Sasaki
, Y. 1958. An objective analysis based on the variational method. J. Meteor. Soc. Japan, 77– 88. -
Sasaki
, Y. 1969. Proposed inclusion of time variation terms, observational and theoretical, in numerical variational objective analysis. J. Meteor. Soc. Japan, 115– 124. -
Stephens
, J. J.and Stitt, J. M.. Optimum influence radii for interpolation with the method of successive corrections. Mon. Wea. Rev. 98, 680– 687. -
Thompson
, P. D. 1969. Reduction of analysis error through constraints of dynamical consistency. J. Appl. Meteor. 8, 738– 742. -
U.S. Dept of Commerce
, 1970. Federal Meteorological Handbook No. 1—Surface Observations. Wash., D.C.: Supt. of Documents, U.S. Print.
DOI: https://doi.org/10.3402/tellusa.v30i6.10395 | Journal eISSN: 3035-9554
Language: English
Page range: 496 - 516
Submitted on: May 31, 1978
Published on: Jan 1, 1978
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1978 John M. Lewis, Stephen C. Bloom, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.