@article{kiefer_lin_charney_2008, title={A study of two-dimensional dry convective plume modes with variable critical level height}, volume={65}, ISSN={["0022-4928"]}, DOI={10.1175/2007JAS2301.1}, abstractNote={Abstract}, number={2}, journal={JOURNAL OF THE ATMOSPHERIC SCIENCES}, author={Kiefer, Michael T. and Lin, Yuh-Lang and Charney, Joseph J.}, year={2008}, month={Feb}, pages={448–469} }
 @article{kaplan_huffman_lux_charney_riordan_lin_2005, title={Characterizing the severe turbulence environments associated with commercial aviation accidents. Part 1: A 44-case study synoptic observational analyses}, volume={88}, ISSN={["1436-5065"]}, DOI={10.1007/s00703-004-0080-0}, number={3-4}, journal={METEOROLOGY AND ATMOSPHERIC PHYSICS}, author={Kaplan, ML and Huffman, AW and Lux, KM and Charney, JJ and Riordan, AJ and Lin, YL}, year={2005}, month={Apr}, pages={129–152} }
 @article{kaplan_huffman_lux_cetola_charney_riordan_lin_waight_2005, title={Characterizing the severe turbulence environments associated with commercial aviation accidents. Part 2: Hydrostatic mesoscale numerical simulations of supergradient wind flow and streamwise ageostrophic frontogenesis}, volume={88}, DOI={10.1007/s00703-004-0079-6}, number={04-Mar}, journal={Meteorology and Atmospheric Physics}, author={Kaplan, M. L. and Huffman, A. W. and Lux, K. M. and Cetola, J. D. and Charney, J. J. and Riordan, A. J. and Lin, Y. L. and Waight, K. T.}, year={2005}, pages={153–173} }
 @article{kaplan_lin_charney_pfeiffer_ensley_decroix_weglarz_2000, title={A terminal area PBL prediction system at Dallas-Fort Worth and its application in simulating diurnal PBL jets}, volume={81}, ISSN={["0003-0007"]}, DOI={10.1175/1520-0477(2000)081<2179:ATAPPS>2.3.CO;2}, abstractNote={Abstract A state–of–the–science meso–b–scale numerical weather prediction model is being employed in a prototype forecast system for potential operational use at the Dallas–Fort Worth International Airport (DFW). The numerical model is part of a unique operational forecasting system being developed to support the National Aeronautics and Space Administration's (NASA) Terminal Area Productivity Program. This operational forecasting system will focus on meso–b–scale aviation weather problems involving planetary boundary layer (PBL) turbulence, and is named the Terminal Area PBL Prediction System (TAPPS). TAPPS (version 1) is being tested and developed for NASA in an effort to improve 1–6–h terminal area forecasts of wind, vertical wind shear, temperature, and turbulence within both stable and convective PBLs at major airport terminal areas. This is being done to enhance terminal area productivity, that is, aircraft arrival and departure throughput, by using the weather forecasts as part of the Aircraft Vort...}, number={9}, journal={BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY}, author={Kaplan, ML and Lin, YL and Charney, JJ and Pfeiffer, KD and Ensley, DB and DeCroix, DS and Weglarz, RP}, year={2000}, month={Sep}, pages={2179–2204} }
 @article{charney_fritsch_1999, title={Discrete frontal propagation in a nonconvective environment}, volume={127}, ISSN={["1520-0493"]}, DOI={10.1175/1520-0493(1999)127<2083:DFPIAN>2.0.CO;2}, abstractNote={Abstract Surface discrete frontal propagation in a wintertime, nonconvective environment is documented using conventional surface and upper-air data and simulated using the PSU–NCAR mesoscale model. Synoptic and mesoscale surface analyses show a cold front associated with a synoptic-scale low-pressure system propagating from northwest to southeast across the central United States. Apparently discrete frontal propagation occurs when the surface front dissipates and a new front forms approximately 500 km ahead of the original front, with no compelling evidence of frontal passage in the intervening space. Upper-air analyses indicate the infusion of three different airstreams into the frontal region, resulting in the formation of a ribbon of low static stability air parallel to and several hundred kilometers in advance of the original front. This static stability structure appears to be involved in the observed evolution of the front. The development of precipitation over the intervening zone between the old ...}, number={9}, journal={MONTHLY WEATHER REVIEW}, author={Charney, JJ and Fritsch, JM}, year={1999}, month={Sep}, pages={2083–2101} }