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2. Seasonal and Local Time Variation in the Observed Peak of the Meteor Altitude Distributions by Meteor Radars.

Author

Dawkins, E. C. M., Janches, D., Stober, G., Carrillo‐Sánchez, J. D., Lieberman, R. S., Jacobi, C., Moffat‐Griffin, T., Mitchell, N. J., Cobbett, N., Batista, P. P., Andrioli, V. F., Buriti, R. A., Murphy, D. J., Kero, J., Gulbrandsen, N., Tsutsumi, M., Kozlovsky, A., Lester, M., Kim, J.‐H., and Lee, C.

Subjects
GREENHOUSE gases, GRAVITY waves, SOLAR cycle, ATMOSPHERIC density, ATMOSPHERE, METEOROIDS, METEOR showers
Abstract

Meteoroids of sub‐milligram sizes burn up high in the Earth's atmosphere and cause streaks of plasma trails detectable by meteor radars. The altitude at which these trails, or meteors, form depends on a number of factors including atmospheric density and the astronomical source populations from which these meteoroids originate. A previous study has shown that the altitude of these meteors is affected by long‐term linear trends and the 11‐year solar cycle related to changes in our atmosphere. In this work, we examine how shorter diurnal and seasonal variations in the altitude distribution of meteors are dependent on the geographical location at which the measurements are performed. We use meteoroid altitude data from 18 independent meteor radar stations at a broad range of latitudes and investigate whether there are local time (LT) and seasonal variations in the altitude of the peak meteor height, defined as the majority detection altitude of all meteors within a certain period, which differ from those expected purely from the variation in the visibility of their astronomical source. We find a consistent LT and seasonal response for the Northern Hemisphere locations regardless of latitude. However, the Southern Hemisphere locations exhibit much greater LT and seasonal variation. In particular, we find a complex response in the four stations located within the Southern Andes region, which indicates that the strong dynamical atmospheric activity, such as the gravity waves prevalent here, disrupts, and masks the seasonality and dependence on the astronomical sources. Plain Language Summary: Small meteoroids burn up high in the Earth's atmosphere producing trails of plasma detectable by ground‐based meteor radar instruments. The altitude at which these trails occur depends on a number of factors including atmospheric density and the astronomical source populations from which these meteoroids originate. Previous work demonstrated that the altitude at which the majority of these meteoroids burn up (termed "peak meteor altitude") is affected by long‐term atmospheric changes, such as those related to greenhouse gas emissions and the 11‐year solar cycle. Here, we focus on shorter timescales and analyze meteoroid altitude data from 18 geographically diverse meteor radars to examine the local time (LT) and seasonal variation in the peak meteor altitudes on a latitude basis. We find a consistent LT and seasonal response among the six Northern Hemisphere meteor radar station locations irrespective of latitude. However, we find a more complex response among the 12 Southern Hemisphere stations with much greater LT and seasonal variation. In particular, we found a complex response in the four stations located within the Southern Andes region, a geographic region known for intense atmospheric gravity wave activity, which acts to mask and disrupt the seasonality and dependence on the astronomical sources. Key Points: Local time (LT) and seasonal variations in the peak meteor height exist, which differ from those expected from astronomical variation aloneThere is a consistent LT and seasonal response in the Northern Hemisphere locations regardless of latitudeA complex response in the Andes region where a strong gravity wave component acts to mask seasonality and dependence on astronomical sources [ABSTRACT FROM AUTHOR]

Published
2024
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3. DMT310, a novel once-weekly topical treatment for patients with moderate-to-severe acne vulgaris: Results of a phase 2b randomized, double-blind, placebo-controlled trial

Author

Eichenfield, Lawrence F., primary, DuBois, Janet C., additional, Gold, Michael H., additional, Nardo, Christopher J., additional, Draelos, Zoe D., additional, Armas, E., additional, DeValle, O., additional, Haber, R.S., additional, Jones, T., additional, Kempers, S.E., additional, Knoepp, T.G., additional, Kuttner, B.J., additional, Lieberman, R., additional, Miller, M.L., additional, Stewart, D.M., additional, and Weinberg, J., additional

Published
2023
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5. Executive Summary of the National Cancer Institute Workshop: Highlights and recommendations.

Author

Lieberman, R, Nelson, WG, Sakr, WA, Meyskens, FL, Klein, EA, Wilding, G, Partin, AW, Lee, JJ, and Lippman, SM

Subjects
Humans, Prostatic Neoplasms, Antineoplastic Agents, Anticarcinogenic Agents, Government, National Institutes of Health (U.S.), United States Food and Drug Administration, Drug Industry, Middle Aged, Interinstitutional Relations, United States, Male, Clinical Trials as Topic, Practice Guidelines as Topic, Biomarkers, Tumor, Urology & Nephrology, Clinical Sciences
Abstract

Prostate cancer chemoprevention represents a relatively new and promising strategy for reducing the immense public health burden of this devastating cancer of men in the United States and Western societies. Chemoprevention is defined as the administration of agents (drugs, biologics, and natural products) that modulate (inhibit) one or more steps in the multistage carcinogenesis process culminating in invasive adenocarcinoma of the prostate. In 2000, there were an estimated 170,000 new cases of prostate cancer and 31,000 deaths in the United States. During the past decade, the National Cancer Institute (NCI) organized the chemoprevention research program and began testing the first generation of promising agents (eg, 4-(hydroxy)-fenretinide [4-HPR], difluoromethylornithine [DFMO], antiandrogens) in high-risk cohorts and launched the first-large scale US phase 3 primary prevention trial, known as Prostate Cancer Prevention Trial (PCPT-1), in 18,000 average-risk men (age more than 55 years and prostate-specific antigen [PSA] less than 3 ng/mL) treated for 7 years with finasteride or placebo. In the summer of 1998, the NCI Prostate Cancer Progress Review Group (PRG) Report to the director of NCI was published in response to the leadership of the prostate cancer advocacy community in conjunction with Congress. To further elucidate and address critical issues identified in this report and to develop a research agenda for the newly created Prostate and Urologic Cancer Research Group in the Division of Cancer Prevention at NCI, the NCI organized the workshop "New Clinical Trial Strategies for Prostate Cancer Chemoprevention." The major objectives were to promote understanding and cooperation among the NCI, US Food and Drug Administration (FDA), academia, pharmaceutical industry, and the public regarding new opportunities for clinical prevention trials for prostate cancer. The workshop was divided into three concurrent breakout panels and a fourth joint integrative panel. The workshop addressed multiple key areas identified in the PRG report in the following panels: (1) Molecular Targets and Promising Agents in Clinical Development; (2) Intermediate Endpoint Biomarkers for Prevention Trials; (3) High-Risk Study Populations for Prevention Trials, and (4) Preventive Clinical Trial Designs and Regulatory Issues. Expert panelists were drawn from leading academic, pharmaceutical, and government scientists in basic research and clinical investigation. Key pharmaceutical, biotechnology, academic, and National Institutes of Health scientists presented overviews of their new agents and products in clinical development (representing the next generation of promising agents). Senior FDA physicians from the Center for Drugs and Center for Biologics presented on current standards for new drug and biologic approval for chemoprevention efficacy. Some of the key topics included recent advances in the state of knowledge of promising agents in the clinic based on molecular targets as well as bottlenecks in drug development for pharmaceutical sponsors; strategic modulable biomarkers that can serve as primary endpoints in phase 1/2 trials to assess preventive efficacy; high-risk cohorts with precancer (high-grade prostatic intraepithelial neoplasia) and representative clinical trial designs that are ready for immediate translation into efficient prevention trials, such as Bayesian sequential monitoring for early assessment of biologic activity and factorial designs for assessment of multiagent combinations. Finally, each expert panel generated recommendations for areas of future research emphasizing opportunities and infrastructure needs.

Published
2001

6. Solar cycle and long-term trends in the observed peak of the meteor altitude distributions by meteor radars

Author

Dawkins, E. C. (E. C. M.), Stober, G. (G.), Janches, D. (D.), Carrillo-Sánchez, J. D. (J. D.), Lieberman, R. S. (R. S.), Jacobi, C. (C.), Moffat-Griffin, T. (T.), Mitchell, N. J. (N. J.), Cobbett, N. (N.), Batista, P. P. (P. P.), Andrioli, V. F. (V. F.), Buriti, R. A. (R. A.), Murphy, D. J. (D. J.), Kero, J. (J.), Gulbrandsen, N. (N.), Tsutsumi, M. (M.), Kozlovsky, A. (A.), Kim, J. H. (J. H.), Lee, C. (C.), Lester, M. (M.), Dawkins, E. C. (E. C. M.), Stober, G. (G.), Janches, D. (D.), Carrillo-Sánchez, J. D. (J. D.), Lieberman, R. S. (R. S.), Jacobi, C. (C.), Moffat-Griffin, T. (T.), Mitchell, N. J. (N. J.), Cobbett, N. (N.), Batista, P. P. (P. P.), Andrioli, V. F. (V. F.), Buriti, R. A. (R. A.), Murphy, D. J. (D. J.), Kero, J. (J.), Gulbrandsen, N. (N.), Tsutsumi, M. (M.), Kozlovsky, A. (A.), Kim, J. H. (J. H.), Lee, C. (C.), and Lester, M. (M.)

Abstract

The mesosphere/lower thermosphere (MLT, 80–100 km) region is an important boundary between Earth’s atmosphere below and space above and may act as a sensitive indicator for anthropogenic climate change. Existing observational and modeling studies have shown the middle atmosphere and the MLT is cooling and contracting because of increasing greenhouse gas emissions. However, trend analyses are highly sensitive to the time periods covered, their length, and the measurement type and methodology used. We present for the first time the linear and 11-year solar cycle responses in the meteor ablation altitude distributions observed by 12 meteor radars at different locations. Decreasing altitudes were seen at all latitudes (linear trends varying from −10.97 to −817.95 m dec⁻¹), and a positive correlation with solar activity was seen for most locations. The divergence of responses at high latitudes indicates an important and complex interplay between atmospheric changes and dynamics at varying time scales.

Published
2023

7. Solar Cycle and Long‐Term Trends in the Observed Peak of the Meteor Altitude Distributions by Meteor Radars

Author

Dawkins, E. C. M., primary, Stober, G., additional, Janches, D., additional, Carrillo‐Sánchez, J. D., additional, Lieberman, R. S., additional, Jacobi, C., additional, Moffat‐Griffin, T., additional, Mitchell, N. J., additional, Cobbett, N., additional, Batista, P. P., additional, Andrioli, V. F., additional, Buriti, R. A., additional, Murphy, D. J., additional, Kero, J., additional, Gulbrandsen, N., additional, Tsutsumi, M., additional, Kozlovsky, A., additional, Kim, J. H., additional, Lee, C., additional, and Lester, M., additional

Published
2023
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8. SPEChpc 2021 Benchmark Suites for Modern HPC Systems

Author

Li, J., Bobyr, A., Boehm, S., Brantley, W., Brunst, H., Cavelan, A., Chandrasekaran, S., Cheng, J., Ciorba, F. M., Colgrove, M., Curtis, T., Daley, C., Ferrato, M., Gimenes De Souza, M., Hagerty, N., Henschel, R., (0000-0002-9935-4428) Juckeland, G., (0000-0003-1761-2591) Kelling, J., Li, K., Lieberman, R., McMahon, K., Melnichenko, E., Ayoub Neggaz, M., Ono, H., Ponder, C., Raddatz, D., Schueller, S., Searles, R., Vasilev, F., Melesse Vergara, V., Wang, B., Wesarg, B., Wienke, S., Zavala, M., Li, J., Bobyr, A., Boehm, S., Brantley, W., Brunst, H., Cavelan, A., Chandrasekaran, S., Cheng, J., Ciorba, F. M., Colgrove, M., Curtis, T., Daley, C., Ferrato, M., Gimenes De Souza, M., Hagerty, N., Henschel, R., (0000-0002-9935-4428) Juckeland, G., (0000-0003-1761-2591) Kelling, J., Li, K., Lieberman, R., McMahon, K., Melnichenko, E., Ayoub Neggaz, M., Ono, H., Ponder, C., Raddatz, D., Schueller, S., Searles, R., Vasilev, F., Melesse Vergara, V., Wang, B., Wesarg, B., Wienke, S., and Zavala, M.

Abstract

The SPEChpc™ 2021 suites are application-based benchmarks de- signed to measure performance of modern HPC systems. The bench- marks support MPI, MPI+OpenMP, MPI+OpenMP target offload, MPI+OpenACC and are portable across all major HPC platforms.

Published
2022

10. APPLICATION OF NEXT GENERATION TECHNOLOGIES

Author

Rojas, L., primary, Ergun, A., additional, Accorsi, A., additional, Sartain, C., additional, Raman, A., additional, Lieberman, R., additional, Valentine, E., additional, Wertz, M., additional, Townsend, E., additional, Wilson, G., additional, Plioudakis, D., additional, Wallace, O., additional, Silver, S., additional, and Moxham, C., additional

Published
2021
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19. A Conjugate Study of Mean Winds and Planetary Waves Employing Enhanced Meteor Radars at Rio Grande, Argentina (53.8degS) and Juliusruh, Germany (54.6degN)

Author

Fritts, D. C, Imura, H, Lieberman, R, Janches, D, and Singer, W

Subjects
Meteorology And Climatology
Abstract

Two meteor radars with enhanced power and sensitivity and located at closely conjugate latitudes (54.6degN and 53.8degS) are employed for inter-hemispheric comparisons of mean winds and planetary wave structures. Our study uses data from June 2008 through May 2010 during which both radars provided nearly continuous wind measurements from approx.80 to 100 km. Monthly mean winds at 53.8degS exhibit a somewhat stronger westward mean zonal jet in spring and early summer at lower altitudes and no westward monthly mean winds at higher altitudes. In contrast, westward mean winds of approx.5-10 m/s at 54.6degN extend to above 96 km during late winter and early spring each year. Equatorward monthly mean winds extend approximately from spring to fall equinox at both latitudes, with amplitudes of approx.5-10 m/s and more rapid decreases in amplitude at 54.6degN at higher altitudes. Meridional mean winds are more variable at both latitudes during fall and winter, with both poleward and equatorward monthly means indicating longer-period variability. Planetary waves seen in the 2-day mean data are episodic and variable at both sites, exhibit dominant periodicities of approx.8-10 and 16-20 days and are more confined to late fall and winter at 54.6degN. At both latitudes, planetary waves in the two period bands coincide closely in time and exhibit similar horizontal velocity covariances that are positive (negative) at 54.6degN (53.8degS) during peak planetary wave responses.

Published
2011

22. 93rd annual convention podium and poster abstracts

Author

Davis, C. M., Strong, S. A., Hellinger, M. D., Williamson, P. R., Larach, S. W., Ferrara, A., Blake, T. B., Medich, D. S., Ziv, Y., Oakley, J. R., Reissman, P., Piccirillo, M., Ulrich, A., Nogueras, J. J., Wexner, S. D., Rubin, M. S., Bodenstein, L. E., Kent, K. C., Williamson, M. E. R., Lewis, W. G., Sagar, P. M., Holdsworth, P. J., Johnston, D., Fazio, V. W., Goldblum, J. R., Sirimarco, M. T., Lavery, I. C., Petras, R. E., Treem, W. R., Cohen, J., Davis, P. M., Hyams, J. S., Eu, K. W., Bartolo, D. C. C., Green, J. D., Riether, R. D., Rosen, L., Stasik, J. J., Sheets, J. A., Reed, J., Khubchandani, I. T., Armitage, N. C., Chapman, M., Hardcastle, J. D., Viamonte, M., Plasencia, G., Wiltz, O., Jacobs, M., Finan, P. J., Passaro, M., Church, J. M., McGannon, E., Wilson, M., Hull-Boiner, S., Kollmorgen, C. F., Meagher, A. P., Wolff, B. G., Pemberton, J. H., Martenson, J. A., Ilstrup, D. M., Moran, M. R., Ramos, A., Rothenberger, D. A., Goldberg, S. M., Johnson, D., Madoff, R. D., Wong, W. D., Finne, III, C. O., Konishi, F., Furuta, K., Kanazawa, K., Lockhart, D., Schmitt, S., Caushaj, P. P., Garcia-Aguilar, J., Belmonte, C., Schiesel, E. C., Mazier, W. P., Senagore, A. J., Piccirillo, M. F., Teoh, T. -A., Yoon, K. -S., Paul, R. A. Patino, Lucas, J., Nelson, R., Norton, N., Cautley, E., Schouten, W. R., Briel, J. W., Auwerda, J. J. A., de Graaf, E. J. R., Lowry, A. C., Sentovich, S. M., Blatchford, G. J., Rivela, L. J., Thorson, A. G., Christensen, M. A., Jorge, J. M. N., Yang, Y. K., Shafik, A., Allendorf, J. D. F., Kayton, M. L., Libutti, S. K., Trokel, M. J., Whelan, R. L., Treat, M. R., Nowygrod, R., Bessler, M., Frank, R. E., Saclarides, T. J., Leurgans, S., Speziale, N. J., Drab, E., Rubin, D., Hull, T. L., Schroeder, T. K., Scholefield, J. H., Ogunbiyi, O. A., Smith, J. H. F., Rogers, K., Sharp, F., Longo, W. E., Vernava, III, A. M., Wade, T. P., Coplin, M. A., Virgo, K. S., Johnson, F. E., Brady, M., Kavolius, J., Quan, S. H. Q., Goldstein, E. T., Feldman, S., Shub, H. A., Bennett, D. R., Kumar, R., McMillen, M. A., Thornton, S., Khoury, D. A., Opelka, F. G., Teoh, T -A., Cohen, S. M., Weiss, E. G., Ortiz, H., De Miguel, M., Armendáriz, P., Rodriguez, J., Chocarro, C., Farouk, R., Dorrance, H. R., Duthie, G. S., Rainey, J. B., Morgado, Jr., P. J., Corman, M. L., Kawamura, Y. J., Sawada, T., Muto, T., Nagai, H., Hill, J., MacLennan, I., Binderow, S. R., Daniel, N., Ehrenpreis, E. D., Jensen, J. E., Bonner, G. F., Ruderman, W. B., Milsom, J. W., Gibbs, D. H., Beck, D. E., Hicks, T. C., Timmcke, A. E., Gathright, Jr, J. B., Cheong, D., Lucas, F. V., McGinity, M., Taylor, B. A., Godwin, P., Holdsworth, P., Lewis, W., Quirke, P., Williamson, M., Kokoszka, J., Pavel, D., Abcarian, H., Stephenson, B. M., Morgan, A. R., Salaman, J. R., Wheeler, M. H., Tran, T. C. K., Willemsen, W., Kuijpers, H. C., Lehman, J. F., Wiseman, J. S., MacFie, J., Sedman, P., May, J., Mancey-Jones, B., Johnstone, D., Nwariaku, F. E., Rochon, R. B., Huber, P. J., Carrico, C. J., Ortega, A., Beart, R., Winchester, D., Steele, G., Green, R., Caushaj, P. F., Devereaux, D., Griffey, S., Reiver, D., Kmiot, W. A., Baker, R., Luchtefeld, M. A., Anthone, G., Schlinkert, R., Roig, J. V., Villoslada, C., Solana, A., Alos, R., Hinojosa, J., Lledo, S., Johnson, D. R. E., Buie, W. D., Jensen, L. L., Heine, J., Hoffmann, B., Timmcke, A., Hicks, T., Opelka, F., Beck, D., Sousa, Jr., A., AraÚjo, S. A., Damico, F. M., Cordeiro, A. C., Pinotti, H. W., Gama, A. H., Fengler, S., Pearl, R., Orsay, C., Seow-Choen, F., Ho, J. M. S., Wiltz, O. H., Torregrosa, M., Brasch, R. C., Bufo, A. J., Krienberg, P., Johnson, G. P., Gowen, G. F., Mullen, P. D., Behrens, D., Hughes, T. G., Wynn, M., Pollack, J. S., Rajagopal, A. S., Huynh, T., Schanbacher, C., Hickson, W. G. E., Yang, Y. -K., Heymen, S., Choi, S. -K., Teoh, T. -A., Wexner, S. D., Vaccaro, C. A., Teoh, T. A., Nogueras, J. J., Choi, S. K., Cheong, D. M. O., Salanga, V. D., MacDonald, A., Baxter, J. N., Finlay, I. G., Mellgren, A., Bremmer, S., Dolk, A., Gillgren, P., Johansson, C., Ahlbäck, S. O., Udén, R., Holmström, B., Ferrara, A., O'Donovan, S., Larach, S. W., Williamson, P. R., Neto, J. A. Reis, Ciquini, S., Quilici, F. A., Reis, Jr., J. A., Torrabadella, L., Salgado, G., Whelan, R. L., Horvath, K. D., Golub, R., Ahsan, H., Cirocco, W., Ziv, Y., Fazio, V. W., Oakley, J. R., Church, J. M., Milsom, J. W., Lavery, L. C., Cohen, S. M., Kmiot, W. A., Reiver, D., Reissman, P., Weiss, E. G., Alós, R., García-Granero, E., Roig, J. V., Uribe, N., Sala, C., Lledo, S., Ozuner, G., Strong, S. A., Bufo, A. J., Daniels, G., Lieberman, R. C., Feldman, S., Lucas, F. V., Longo, W. E., Polites, G., Deshpande, Y., Vernava, A. M., Niehoff, M., Chandel, B., Berglund, D. D., Madoff, R. D., Gemlo, B. T., Spencer, M. P., Goldberg, S. M., Lowry, A. C., Marcello, P. W., Roberts, P. L., Schoetz, D. J., Murray, J. J., Coller, J. A., Veidenheimer, M. C., Koltun, W. A., Bloomer, M. M., Colony, P., Ruggeiro, F., Fleshner, P. R., Michelassi, F., Lewis, W., Williamson, M., Holdsworth, P., Finan, P., Ash, D., Johnston, D., Moran, M. R., Ramos, A., Rothenberger, D. A., Antonenko, D. R., Khanduja, K. S., Fitzgerald, S. D., Meagher, A. P., Moniz-Pereira, P., Wolff, B. G., Outwater, E. K., Marks, G. J., Mohiuddin, M., Sagar, P. M., Hartley, M. N., Mancey-Jones, B., Sedman, P., May, J., MacFie, J., Holbrook, R. F., Rodriguez-Bigas, M. A., Ramakrishnan, K., Palmer, M. L., Petrelli, N. J., Takahashi, T., Nivatvongs, S., Batts, K. P., Lucas, S. W., Klein, S. N., Keidan, R. D., Bannon, J. P., Zhou, J., Armitage, N. C., Hunt, L. M., Robinson, M. H., Hugkulstone, C. E., Clarke, B., Vernon, S. A., Gregson, R. H., Hardcastle, J. D., Ryan, M., Dutta, S., Levine, A., Ortega, A., Anthone, G., Beart, R., Dominguez, J. M., Saclarides, T. J., Bolan, P., Bines, S. D., Adachi, M., Watanabe, T., Sawada, T., Okinaga, K., Muto, T., Hase, K., Shatney, C., Mochizuki, H., Johnson, D., Ure, T., Dehghan, K., Andrus, C. A., Daniel, G. L., D'Emilia, J. C., Rodriguez-Bigas, M., Suh, O. K., Brewer, D. A., Fung, C., Chapuis, P., Bokey, E. L., Garcia, J. C., Banerjee, S., Remzi, F. H., Lavery, I. C., Jorge, J. M. N., Ger, G. C., Gonzalez, L., Gee, A. S., Roe, A. M., Durdey, P., Kaye, M. D., Kyzer, S., Gordon, P. H., Hasegawa, M., Bun, P. Tae, Ikeuchi, D., Onodera, H., Imamura, M., Maetani, S., Blake, T., Hellinger, M., Grewal, H., Klimstra, D. S., Cohen, A. M., Guillem, J. G., Rooney, P. S., Gifford, K. -A., Clarke, P. A., Kuhn, J. A., Bryce, K., Frank, N., Dignan, R. D., Lichliter, W. E., Franko, E., Jacobson, R. M., Preskitt, J. T., Lieberman, Z., Tulanon, P., Steinbach, H., McCarty, T., Simons, T., Plasencia, G., Viamonte, M., Wiltz, O., Jacobs, M., Chen, W. S., Leu, S. Y., Hsu, H., Bessler, M., Halverson, A., Kayton, M. L., Treat, M. R., Nowygrod, R., Congilosi, S., Madoff, R., Wong, W. D., Rothenberger, D., Buie, W. D., Paterson, R., Cartmill, J. A., Trokel, M. J., Gingold, B. S., Cooper, M., Gorfine, S. R., Bauer, J. J., Gelernt, I. M., Kreel, I., Harris, M. T., Vallejo, J. F., Kestenberg, A., Miyajima, N., Kano, N., Ishikawa, Y., Sakai, S., Yamakawa, T., Otchy, D. P., Van Heerden, J. A., Ilstrup, D. M., Weaver, A. L., Winter, L. D., Mav, J., Lee, P. Y., Vetto, J. T., Sullivan, E. S., Rabkin, J., Mayoral, J. L., Matas, A. J., Bove, P., Visser, T., Barkel, D., Villalba, M., Bendick, P., Glover, J., Golub, R. W., Cirocco, W. C., Daniel, N., Altringer, W., Domingues, J. M., Brubaker, L. T., Smith, C. S., Kumar, S., and Gilbert, P.

Published
1994
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23. Podium presentations

Author

Foley, E. F., Marcello, P. W., Roberts, P. L., Murray, J. J., Coller, J. A., Veidenheimer, M. C., Schoetz, D. J., McIntyre, P. B., Pemberton, J. H., Wolff, B. G., Beart, Jr., R. W., Kelly, K. A., Dozois, R. R., Sugita, A., Fukushima, T., Harada, H., Yamamoto, M., Shimada, H., Tjandra, J. J., Fazio, V. W., Milson, J. W., Lavery, I. C., Oakley, J. R., Fabre, J. M., Karch, L. A., Bauer, J. J., Gorfine, S. R., Gelernt, I. M., Metcalf, A. M., Varilek, G., Keck, J. O., Hoffmann, D. C., Sgambati, S. A., Sardella, W. V., Marts, B. C., Longo, W. E., Vernava, III, A. M., Kennedy, D. J., Daniel, G. L., Jones, I., Venkatesh, K. S., Diamond, L. W., Larson, D. M., Ramanujam, P. J., Hicks, J. R., Ellis, C. N., Blakemore, W. S., Nathanson, S. D., Linden, M. D., Tender, P., Zarbo, R. J., Nelson, L., Bannon, J., Marks, G., Zhou, J., Mohiuddin, M., Marks, J., Pollard, C. W., Nivatvongs, S., Rojanasakul, A., Ilstrup, D. M., Speziale, N. J., Saclarides, T. J., Rubin, D. B., Szeluga, D. J., Morgado, P. J., Gomez, L. G., Morgado, Jr., P. J., Neto, J. A. Reis, Quilici, F. A., Cordeiro, F., Reis, Jr., J. A., Nitecki, S., Benn, P., Sarr, M. G., Weiland, L. H., Elhadad, A., Rouffet, F., Baillet, P., Akasu, T., Moriya, Y., Hojo, K., Sugihara, K., Oshima, H., Liu, S. K., Church, J. M., Kirkpatrick, J. R., Danielson, C. L., Dominguez, J. M., Jakate, S. M., Savin, M. H., Altringer, W. J., Lee, C. S., Spencer, M. P., Madoff, R. D., Barrett, R. C., Oster, M. A., Durdey, P., Stein, B. L., Staniunas, R. J., Grewal, H., Guillem, J. G., Quan, S., Enker, W. E., Cohen, A. M., van Tets, W. F., Kuijpers, H. C., Kerner, B. A., Wise, Jr., W. E., Golub, R. W., Arnold, M. W., Aguilar, P. S., Pernikoff, B. J., Eisenstat, T. E., Rubin, R. J., Oliver, G. C., Salvati, E. P., Lunniss, P. J., Sultan, A. H., Barker, P. G., Armstrong, P., Bartram, C. I., Phillips, R. K. S., Schouten, W. R., Briel, J. W., Auwerda, J. J. A., Harnsberger, J. R., Robbins, P. L., Brabbee, G. W., Ryhammer, A. M., Bek, K. M., Hanberg-Sørensen, F., Laurberg, S., Hoff, S. D., Bailey, H. R., Butts, D. R., Max, E., Smith, K. W., Zamora, L. F., Skakun, G. B., Khanduja, K. S., Lee, H., Beart, R. W., Spencer, R., Wiseman, J. S., Senagore, A. J., Bain, I. M., Oliff, J., Min, L., Neoptolomos, J., Keighley, M. R. B., O'Kelly, T. J., Davies, J., Brading, A. F., Mortensen, N. J. McC, Park, J. -G., Han, H. J., Kang, M. S., Nakamura, Y., Goldberg, G. S., Orkin, B. A., Smith, L. E., Fleshner, P. R., Freilich, M. I., Meagher, A. P., Adams, W. J., Lubowski, D. Z., King, D. W., Moran, M., Opelka, F., Timmcke, A., Hicks, T., Gathright, Jr., J. B., Leu, S. Y., Hsu, H., Dean, P. A., Ramsey, P. S., Nelson, H., Philpott, G., Siegel, B., Schwarz, S., Fleshman, J., Welch, M., Connett, J., Buie, W. D., Johnson, D. R., Heine, J. A., Wong, W. D., Rothenberger, D. A., Goldberg, S. M., Shafik, A., MacDonald, A., Craig, J. W., Finlay, I. G., Baxter, J. N., Muir, T. C., Parikh, S., Gold, R. P., Gottesman, L., Annibali, R., Öresland, T., Hallgren, T., Fasth, S., Hultén, L., Farouk, R., Duthie, G. S., MacGregor, A. B., Bartolo, D. C. C., Williamson, M. E. R., Lewis, W. G., Holdsworth, P. J., Hall, N., Finan, P. J., Johnston, D., Seow-Choen, F., Goh, H. S., Motson, R. W., Walsh, C. J., Mooney, E., Yamashita, H. J., Wise, W. E., Hartmann, R. F., Seccia, M., Menconi, C., Ghiselli, G., Cavina, E., Salomon, M. C., Ferrara, A., Larach, S. W., Williamson, P. R., Bass, E. M., Orsay, C. P., Firfer, B., Ramakrishnan, V., Abcarian, H., Bufo, A. J., Feldman, S., Daniels, G. A., Lieberman, R. C., Loder, P. B., Kamm, M. A., Nicholls, R. J., Kum, C. K., Ngoi, S. S., Goh, P. M. Y., Tekant, Y., Isaac, J. R., Gerstle, J. T., Kauffman, G. L., and Koltun, W. A.

Published
1993
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24. Observations of Intermediate-Scale Diurnal Waves in the Equatorial Mesosphere and Lower Thermosphere

Author

Lieberman, R. S, Riggin, D. M, Garcia, R. R, Wu, Qian, and Remsberg, E. E

Subjects
Geophysics
Abstract

The purpose of this study is to seek observational evidence for diurnal, vertically propagating inertia-gravity waves (IGWs) in the mesosphere and lower thermosphere (MLT). Numerical modeling studies indicate that vertically propagating IGWs excited by tropical heating provide a significant source of momentum for the semiannual oscillation (SAO) in the equatorial zonal mean winds. The power spectrum of these waves has a strong diurnal component. We analyze global patterns of ascending and descending node differences in MLT satellite temperatures, which are assumed in this study to be proxies for waves of diurnal period. Juxtaposed upon the planetary-scale features are localized variations with longitudinal wavelengths ranging from 25 deg to 50 deg, and with vertical wavelengths between 13 and 25 km. These intermediate-scale variations are spatially coherent, and persist for several weeks. Their amplitudes generally increase with altitude, while their phase structures suggest both eastward and westward propagation. The variance of wave numbers 9-17 in the MLT is examined in relation to the underlying stratospheric zonal mean zonal gradient winds. Stronger variances generally coincide with periods where the underlying zonal mean winds are relatively light, or unidirectional. The weak inverse association between variance strength and zonal wind magnitude is suggestive of a wave filtering mechanism.

Published
2006
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27. Development and validation of an instrument to measure occupational stress in speech-language pathologists

Author

Fimian, Michael J., Lieberman, R. Jane, and Fastenau, Philip S.

Subjects
Psychological tests -- Validity, Speech therapists -- Psychological aspects, Stress (Psychology) -- Testing, Burn out (Psychology) -- Testing, Health, Languages and linguistics
Abstract

The Speech-Language Pathologist Stress Inventory (SLPSI) is a 48-item questionnaire adapted from the Teacher Stress Inventory (Fimian, 1988). Factor analyses of the responses of 626 speech-language pathologists revealed four stress source factors (Bureaucratic Restrictions, Time and Workload Management, Lack of Professional Supports, and Instructional Limitations) and two stress manifestation factors (Emotional-Fatique Manifestations and Bio-behavioral Manifestations). The internal consistency reliability of scales based on these factors ranged from .71 to .87, with .93 for the entire scale. Evidence for construct validity was found in moderate positive correlations between the scales of the SLPSI and the scales of the Maslach Burnout Inventory (MBI) (Maslach & Jackson, 1986). Stress and burnout subscale intercorrelations ranged from .10 to .82 (p

Published
1991

28. Development of an Early Warning Fire Detection System using Correlation Spectroscopy

Author

Goswami, K, Voevodkin, G, Rubstov, V, Lieberman, R, and Piltch, N

Subjects
Inorganic, Organic And Physical Chemistry
Abstract

Combustion byproducts are numerous. A few examples of the gaseous byproducts include carbon dioxide, carbon monoxide, hydrogen chloride, hydrogen cyanide and ammonia. For detecting these chemical species, classic absorption spectroscopy has been used for many decades, but the sensitivity of steady-state methods is often unsuitable for the detection of trace compounds at the low levels (parts per million to parts per billion) appropriate for scientific purposes. This is particularly so for monitoring equipment, which must be compact and cost-effective, and which is often subjected to shock, vibration, and other environmental effects that can severely degrade the performance of high-sensitivity spectrometers in an aircraft. Steady-state techniques also suffer from a lack of specificity; the deconvolution of the spectra of complex mixtures is a laborious and error prone process. These problems are exacerbated in remote fiber-optic monitoring where, for practical reasons, the fundamental absorbance region of the spectrum (often between 3 and 8 microns) is inaccessible, and the low-strength, closely spaced, near-infrared overtone absorbance bands must be used. We circumvented these challenges by employing correlation spectroscopy, a variation of modulation spectroscopy.

Published
2001

33. Observations of the diurnal tide from space

Author

Hays, Paul B, Wu, D. L, Burrage, M. D, Gell, D. A, Grassl, H. J, Lieberman, R. S, Marshall, A. R, Morton, Y. T, Ortland, D. A, and Skinner, W. R

Subjects
Geosciences (General)
Abstract

This study presents a climatology of mesospheric and lower-thermospheric diurnal tidal winds obtained with the High Resolution Doppler Imager (HRDI) on the Upper Atmosphere Research Satellite (UARS). The observations reveal that although tidal structures are present at all times, like the prevailing zonal winds, they exhibit significant semiannual as well as other shorter-term variations in amplitude. Results are presented for a period extending over more than one year from November 1991 to July 1993. The 1,1 diurnal tidal amplitude of the meridional component, characterized by the value at an altitude of 90 km and a latitude of 22 deg, ranges from a minimum at solstice of less than 20 m per sec to an equinox maximum of over 70 m per sec. The vertical wavelength and phase of the tide show only slight variations throughout the year, with a suggestion of semiannual variations in both.

Published
1994
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34. Observations of the quasi 2-day wave from the High Resolution Doppler Imager on UARS

Author

Wu, D. L, Hays, P. B, Skinner, W. R, Marshall, A. R, Burrage, M. D, Lieberman, R. S, and Ortland, D. A

Subjects
Geophysics
Abstract

A strong westward traveling oscillation, with a period of 2 days and zonal wave number 3, is observed in the mesospheric and lower thermospheric winds from the High Resolution Doppler Imager (HRDI) on the Upper Atmosphere Research Satellite (UARS). The important events happen in January, July, and September/October, of which the occurrence in January is the strongest with an amplitude over 60 m/s. Detailed analyses for the periods of January 1992 and January 1993 reveal a cause-and-effect relationship in the wave developing process at 95 km. The global structures of the wave amplitude and phase are also presented.

Published
1993

35. Zonal mean winds in the equatorial mesosphere and lower thermosphere observed by the High Resolution Doppler Imager

Author

Lieberman, R. S, Burrage, M. D, Gell, D. A, Hays, P. B, Marshall, A. R, Orthland, D. A, Skinner, W. R, Wu, D. L, Vincent, R. A, and Franke, S. J

Subjects
Geophysics
Abstract

This paper presents analyses of mesospheric and lower thermospheric zonal mean winds observed by the High Resolution Doppler Imager (HRDI) on the Upper Atmosphere Research Satellite (UARS). Monthly averages of the equatorial zonal mean zonal winds are presented for January 1992 through June 1993. Equatorial zonal winds in the 70-90 km region are dominated by a semiannual oscillation (SAO), ranging from 30 m/s (westerly) to -100 m/s (easterly). At high latitudes the zonal wind variations are predominantly annual. Above 90 km, the low-latitude flow is easterly at all times, punctuated by a small semiannual variation. This behavior may be related to the deposition of momentum by the diurnal tides.

Published
1993

36. Comparison of HRDI wind measurements with radar and rocket observations

Author

Burrage, M. D, Skinner, W. R, Marshall, A. R, Hays, P. B, Lieberman, R. S, Franke, S. J, Gell, D. A, Ortland, D. A, Morton, Y. T, and Schmidlin, F. J

Subjects
Meteorology And Climatology
Abstract

Wind fields in the mesosphere and lower thermosphere are obtained with the High Resolution Doppler Imager (HRDI) on the Upper Atmosphere Research Satellite (UARS) by observing the Doppler shifts of emission lines in the O2 Atmospheric band. The validity of the measured winds depends on an accurate knowledge of the positions on the detector of the observed lines in the absence of a wind-induced Doppler shift. These positions have been determined to an accuracy of approximately 5 m/s from the comparison of winds measured by HRDI with those obtained by MF radars. Excellent agreement is found between HRDI measured winds and winds observed with radars and rockets. In addition, the sensitivity of HRDI to migrating tides and other large scale waves is demonstrated.

Published
1993

37. Optical fiber sensors for life support applications

Author

Lieberman, R. A, Schmidlin, E. M, Ferrell, D. J, and Syracuse, S. J

Subjects
Instrumentation And Photography
Abstract

Preliminary experimental results on systems designed to demonstrate sensor operation in regenerative food production and crew air supply applications are presented. The systems use conventional fibers and sources in conjunction with custom wavelength division multiplexers in their optical signal processing sections and nonstandard porous optical fibers in the optical sensing elements. It is considered to be possible to create practical sensors for life-support system applications, and particularly, in regenerative food production environments, based on based on reversible sensors for oxygen, carbon monoxide, and humidity.

Published
1992

38. Communication Strategies Used By Language-Impaired and Language-Normal Children.

Author

Lieberman, R. Jane and Hutchinson, Edward C.

Abstract

The acquisition of communicative competence is explored in a study of the emergence of functional use of language among early school-aged children. Cognitive communication strategies and language use in the context of early academic success or lack of success are discussed. Results are presented. (DF)

Published
1984

39. Content Relevance and Content Coverage in Tests of Grammatical Ability.

Author

Lieberman, R. Jane and Michael, Ann

Abstract

Three tests of grammatical ability (Carrow Elicited Language Inventory, Test of Language Development, and Clinical Evaluation of Language Functions) were evaluated for content-oriented test construction. Content domains were found deficient when judged against an external standard as well as when examined according to their own content specifications. (Author/CL)

Published
1986

40. A Comparison of Four Adolescent Language Tests.

Author

Lieberman, R. Jane

Abstract

While no significant differences were found for sixth-graders' (N=30) performance on the Fullerton Test for Adolescents, Test of Adolescent Language, and the Clinical Evaluation of Language Functions, significantly fewer students were identified as needing further evaluation by the Screening Test of Adolescent Language than by the other three tests. (Author/CB)

Published
1987

45. Intravenous Angiography Using Computerized Fluoroscopy Apparatus

Author

Mistretta, Charles A., Kruger, Robert A., Ergun, David L., Shaw, Chorng Gang, Strother, C. M., Crummy, A. B., Sackett, J. F., Myerowitz, D., Turnipseed, W., Van Lysel, M., Zarnstorff, W., Lieberman, R., Ruzicka, F. F., Lindberg, D. A. B., editor, Reichertz, P. L., editor, Sklansky, Jack, editor, and Bisconte, Jean-Claude, editor

Published
1982
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47. Ironies of the American State

Author

King, D and Lieberman, R

Abstract

“Ironies of the American State” (with Robert C Lieberman), World Politics 61 (July 2009) 547-588.

Published
2016

48. American State Building: The Theoretical Challenge

Author

King, D and Lieberman, R

Abstract

“American State Building: The Theoretical Challenge” (with Robert C Lieberman) in The Unsustainable American State eds Lawrence Jacobs and Desmond King New York: Oxford University Press, 2009.

Published
2016

49. American Political Development as a Process of Democratization

Author

King, D, Lieberman, R, and King et al, D

Abstract

“American Political Development as a Process of Democratization,” with Robert C Lieberman, in Democratization in America: A Comparative Historical Analysis, Eds. Desmond King et al. Baltimore: Johns Hopkins University Press, 2009.

Published
2016

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