Relevant bibliographies by topics / Atmosphere response

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Atmosphere response'

Author: Grafiati
Published: 2 June 2025
Last updated: 31 July 2025

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Journal articles on the topic "Atmosphere response"

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Zakharov, Viktor, Maria Solovieva, Sergey Shalimov, Mirseid Akperov, Galiya Korkina, and Nadezhda Bulatova. "Upper atmosphere response to extratropical cyclones." Solar-Terrestrial Physics 11, no. 1 (2025): 70–80. https://doi.org/10.12737/stp-111202509.

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We have examined the response of the lower and upper ionosphere to the passage of extratropical cyclones in 2014–2023, using measurements made at regional ultra-long-wave radio stations and satellites of the Swarm mission in the Far Eastern region of Russia. For twelve cyclones, we have found that disturbances in the lower ionosphere, observed in VLF signal amplitude and phase variations, as well as their associated electron density variations in the upper ionosphere during the active stage of the cyclones, correspond to the passage of atmospheric internal gravity waves and their dissipation,
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Zhao-Jun, Ban, Zhang Jing-Lin, Wang Yong-Jiang, et al. "Nutritional Quality of Red Dates (Zizyphus Jujube Mill.) in Response to Modified and Controlled Atmospheric Storage Conditions." Current Topics in Nutraceutical Research 18, no. 1 (2018): 46–51. http://dx.doi.org/10.37290/ctnr2641-452x.18:46-51.

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Quality maintenance and ethanol metabolism of red date (Zizyphus jujube Mill.) fruits in response to modified atmosphere and controlled atmosphere (7% CO<sub>2</sub>, 3% O<sub>2</sub> plus 90% N<sub>2</sub>) were investigated in the present study. Results showed that modified atmosphere and controlled atmosphere significantly maintained higher titratable and ascorbic acid contents during storage at 0°C for 32 days. In addition, ethanol accumulation and alcohol dehydrogenase activity indicated that ethanol metabolism in red dates was substantially inhibited by modified and controlled atmospheri
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Laguë, Marysa M., Gordon B. Bonan, and Abigail L. S. Swann. "Separating the Impact of Individual Land Surface Properties on the Terrestrial Surface Energy Budget in both the Coupled and Uncoupled Land–Atmosphere System." Journal of Climate 32, no. 18 (2019): 5725–44. http://dx.doi.org/10.1175/jcli-d-18-0812.1.

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Abstract Changes in the land surface can drive large responses in the atmosphere on local, regional, and global scales. Surface properties control the partitioning of energy within the surface energy budget to fluxes of shortwave and longwave radiation, sensible and latent heat, and ground heat storage. Changes in surface energy fluxes can impact the atmosphere across scales through changes in temperature, cloud cover, and large-scale atmospheric circulation. We test the sensitivity of the atmosphere to global changes in three land surface properties: albedo, evaporative resistance, and surfac
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Frankignoul, Claude, Nadine Chouaib, and Zhengyu Liu. "Estimating the Observed Atmospheric Response to SST Anomalies: Maximum Covariance Analysis, Generalized Equilibrium Feedback Assessment, and Maximum Response Estimation." Journal of Climate 24, no. 10 (2011): 2523–39. http://dx.doi.org/10.1175/2010jcli3696.1.

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Abstract Three multivariate statistical methods to estimate the influence of SST or boundary forcing on the atmosphere are discussed. Lagged maximum covariance analysis (MCA) maximizes the covariance between the atmosphere and prior SST, thus favoring large responses and dominant SST patterns. However, it does not take into account the possible SST evolution during the time lag. To correctly represent the relation between forcing and response, a new SST correction is introduced. The singular value decomposition (SVD) of generalized equilibrium feedback assessment (GEFA–SVD) identifies in a tru
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Verma, Tarun, R. Saravanan, P. Chang, and S. Mahajan. "Tropical Pacific Ocean Dynamical Response to Short-Term Sulfate Aerosol Forcing." Journal of Climate 32, no. 23 (2019): 8205–21. http://dx.doi.org/10.1175/jcli-d-19-0050.1.

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Abstract The large-scale and long-term climate impacts of anthropogenic sulfate aerosols consist of Northern Hemisphere cooling and a southward shift of the tropical rain belt. On interannual time scales, however, the response to aerosols is localized with a sizable imprint on local ocean–atmosphere interaction. A large concentration of anthropogenic sulfates over Asia may impact ENSO by modifying processes and interactions that generate this coupled ocean–atmosphere variability. Here, we use climate model experiments with different degrees of ocean–atmosphere coupling to study the tropical Pa
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Petricca, Flavio, Antonio Genova, Sander Goossens, Luciano Iess, and Giorgio Spada. "Constraining the Internal Structures of Venus and Mars from the Gravity Response to Atmospheric Loading." Planetary Science Journal 3, no. 7 (2022): 164. http://dx.doi.org/10.3847/psj/ac7878.

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Abstract The gravity fields of celestial bodies that possess an atmosphere are periodically perturbed by the redistribution of fluid mass associated with atmospheric dynamics. A component of this perturbation is due to the gravitational response of the body to the deformation of its surface induced by the atmospheric pressure loading. The magnitude of this effect depends on the relation between the loading and the response in terms of geopotential variations measured by the load Love numbers. In this work, we simulate and analyze the gravity field generated by the atmospheres of Venus and Mars
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Grankin, Dmitry, Irina Mironova, Galina Bazilevskaya, Eugene Rozanov, and Tatiana Egorova. "Atmospheric Response to EEP during Geomagnetic Disturbances." Atmosphere 14, no. 2 (2023): 273. http://dx.doi.org/10.3390/atmos14020273.

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Energetic electron precipitation (EEP) is associated with solar activity and space weather and plays an important role in the Earth’s polar atmosphere. Energetic electrons from the radiation belt precipitate into the atmosphere during geomagnetic disturbances and cause additional ionization rates in the polar middle atmosphere. These induced atmospheric ionization rates lead to the formation of radicals in ion-molecular reactions at the heights of the mesosphere and upper stratosphere with the formation of reactive compounds of odd nitrogen NOy and odd hydrogen HOx groups. These compounds are
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Liu, Zhengyu, Yun Liu, Lixin Wu, and R. Jacob. "Seasonal and Long-Term Atmospheric Responses to Reemerging North Pacific Ocean Variability: A Combined Dynamical and Statistical Assessment*." Journal of Climate 20, no. 6 (2007): 955–80. http://dx.doi.org/10.1175/jcli4041.1.

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Abstract The atmospheric response to a North Pacific subsurface oceanic temperature anomaly is studied in a coupled ocean–atmosphere general circulation model using a combined dynamical and statistical approach, with the focus on the evolution at seasonal and longer time scales. The atmospheric response is first assessed dynamically with an ensemble coupled experiment. The atmospheric response is found to exhibit a distinct seasonal evolution and a significant long-term response. The oceanic temperature anomaly reemerges each winter to force the atmosphere through an upward heat flux, forcing
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Agarwal, Neeraj, Armin Köhl, Carlos Roberto Mechoso, and Detlaf Stammer. "On the Early Response of the Climate System to a Meltwater Input from Greenland." Journal of Climate 27, no. 21 (2014): 8276–96. http://dx.doi.org/10.1175/jcli-d-13-00762.1.

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Abstract The early response of the atmosphere–ocean system to meltwater runoff originating from the Greenland ice sheet is studied using a coupled atmosphere–ocean general circulation model (AOGCM). For this purpose, AOGCM ensemble simulations without and with associated ocean freshening around Greenland are compared. For freshwater perturbations initiated in northern winter, the mean response for the first three months shows the emergence of negative sea surface temperature (SST) anomalies in the Denmark Strait, in association with enhanced oceanic advection by the East Greenland Current. The
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KASTING, J. F., and T. P. ACKERMAN. "Response: Earth's Early Atmosphere." Science 235, no. 4787 (1987): 415b. http://dx.doi.org/10.1126/science.235.4787.415b.

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Dissertations / Theses on the topic "Atmosphere response"

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Fan, Meizhu. "Low frequency North Atlantic SST variability weather noise forcing and coupled response /." Fairfax, VA : George Mason University, 2008. http://hdl.handle.net/1920/3421.

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Thesis (Ph.D.)--George Mason University, 2008.<br>Vita: p. 190. Thesis director: Edwin K. Schneider. Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Climate Dynamics. Title from PDF t.p. (viewed Mar. 9, 2009). Includes bibliographical references (p. 181-189). Also issued in print.
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Song, Qingtao. "Surface wind response to oceanic fronts /." View online ; access limited to URI, 2006. http://0-wwwlib.umi.com.helin.uri.edu/dissertations/dlnow/3225330.

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Arnone, Enrico. "The response of the middle atmosphere to regional ozone perturbations." Thesis, University of Leicester, 2007. http://hdl.handle.net/2381/30589.

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The existence of downward propagation mechanisms that couple stratospheric disturbances to the troposphere motivated the study of processes that can influence these stratospheric regimes. The dependence of the variability on the amplitude of the tropospheric wave forcing was studied on a stratosphere-mesosphere model, showing the atmosphere to be at a transition phase between the two regimes, with potential large amplification of the response to small perturbations. The recent discovery of transient luminous events (TLEs) such as sprites motivated the systematic study of the response of the mi
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Screen, James Alexander. "The coupled atmosphere-ocean response to the southern annnular mode." Thesis, University of East Anglia, 2009. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.492928.

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Hughes, John K. "The dynamic response of the global atmosphere-vegetation coupled system." Thesis, University of Reading, 2004. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.397768.

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Call, David A. "An analysis of ice storm impacts, warnings, and emergency management response." Related electronic resource:, 2007. http://proquest.umi.com/pqdweb?did=1398609361&sid=2&Fmt=2&clientId=3739&RQT=309&VName=PQD.

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Zhao, Zhiling. "The Response of O(1S) and OH Emission Brightness to Gravity Wave Perturbations." University of Cincinnati / OhioLINK, 2001. http://rave.ohiolink.edu/etdc/view?acc_num=ucin989251411.

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Moore, Matthew J. "Evolution of boundary layer height in response to surface and mesoscale forcing." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2005. http://library.nps.navy.mil/uhtbin/hyperion/05Mar%5FMoore.pdf.

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Geiger, Felix [Verfasser]. "Fast-response measurements of organic trace species in the Earth's atmosphere / Felix Geiger." Karlsruhe : KIT Scientific Publishing, 2015. http://www.ksp.kit.edu.

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Hood, Lon L., and Boris E. Soukharev. "The Lower-Stratospheric Response to 11-Yr Solar Forcing: Coupling to the Troposphere–Ocean Response." American Meteorological Society (Boston, MA), 2012. http://hdl.handle.net/10150/623318.

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The origin of the tropical lower-stratospheric response to 11-yr solar forcing and its possible coupling to a troposphere–ocean response is investigated using multiple linear regression (MLR) analyses of stratospheric ozone and temperature data over the 1979–2009 period and tropospheric sea level pressure (SLP) data over the 1880–2009 period. Stratospheric MLR results, comparisons with simulations from a chemistry–climate model, and analyses of decadal variations of meridional eddy heat flux indicate that the tropical lower-stratospheric response is produced mainly by a solar-induced modulatio
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Books on the topic "Atmosphere response"

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Kilau, H. W. Capillary wetting response of coal after exposure to ambient air atmosphere. U.S. Dept. of the Interior, Bureau of Mines, 1989.

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Kilau, H. W. Capillary wetting response of coal after exposure to ambient air atmosphere. Dept. of the Interior, 1989.

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Giese, Benjamin S. Equatorial oceanic response to forcing on time scales from days to months. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Pacific Marine Environmental Laboratory, 1989.

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1949-, Noda A., and Kokuritsu Kankyō Kenkyūjo. Chikyū Kankyō Kenkyū Sentā., eds. A new meteorological research institute coupled GCM (MRI-CGCM2): Transient response to greenhouse gas and aerosol scenarios. Center for Global Environmental Research, National Institute for Environmental Studies, Environment Agency of Japan, 2001.

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United States. National Aeronautics and Space Administration., ed. Response of the upper atmosphere to variations in the solar soft X-ray irradiance. National Aeronautics and Space Administration, 1995.

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Fischer, Albert Sok. The upper ocean response to the monsoon in the Arabian Sea. Massachusetts Institute of Technology, 2000.

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Alexander, M. J. The gravity wave response above deep convection in a squall line simulation. National Aeronautics and Space Administration, 1995.

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Alexander, M. J. The gravity wave response above deep convection in a squall line simulation. National Aeronautics and Space Administration, 1995.

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COARE-98 (1998 Boulder, Colo.). COARE-98: Proceedings of a conference on the TOGA Coupled Ocean-Atmosphere Response Experiment (COARE) : Boulder, Colorado, USA, 7-14 July 1998. World Climate Research Programme, 1999.

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COARE 98 (Conference) (1998 Boulder, Colorado). COARE-98: Proceedings of a conference on the TOGA coupled ocean-atmosphere response experiment (COARE), Boulder, Colorado, USA, 7-14 July 1998. [World Climate Research Programme], 1999.

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Book chapters on the topic "Atmosphere response"

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Balasubramanian, Sridhar. "An Experimental Approach Toward Modeling Atmosphere and Ocean Mixing Processes." In Climate Change Signals and Response. Springer Singapore, 2018. http://dx.doi.org/10.1007/978-981-13-0280-0_8.

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Newton, E. K., A. G. Emslie, and John T. Mariska. "Dynamical Response of the Solar Atmosphere to Flare Heating." In Magnetodynamic Phenomena in the Solar Atmosphere. Springer Netherlands, 1996. http://dx.doi.org/10.1007/978-94-009-0315-9_138.

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Dempsey, Jerome A. "Problems with the Hyperventilatory Response to Exercise and Hypoxia." In Oxygen Transfer from Atmosphere to Tissues. Springer US, 1988. http://dx.doi.org/10.1007/978-1-4684-5481-9_24.

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Howarth, Robert W., Renee Santoro, and Anthony Ingraffea. "Chapter 9 Venting and Leaking of Methane from Shale Gas Development: Response to Cathles et al." In Pollution and the Atmosphere. Apple Academic Press, 2016. http://dx.doi.org/10.1201/9781315365633-10.

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Fuller-Rowell, Timothy J. "Storm-Time Response of the Thermosphere–Ionosphere System." In Aeronomy of the Earth's Atmosphere and Ionosphere. Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-94-007-0326-1_32.

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Milanolo, Simone. "Cave Atmosphere Response to Artificial Input of Carbon Dioxide." In Sources and Transport of Inorganic Carbon in the Unsaturated Zone of Karst. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-29308-0_7.

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Fels, Stephen B. "Response of the Middle Atmosphere to Changing O3 and CO2 — A Speculative Tutorial." In Transport Processes in the Middle Atmosphere. Springer Netherlands, 1987. http://dx.doi.org/10.1007/978-94-009-3973-8_24.

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Smith, William H. "The Atmosphere and the Rhizosphere: Linkages with Potential Significance for Forest Tree Health." In Mechanisms of Forest Response to Acidic Deposition. Springer New York, 1990. http://dx.doi.org/10.1007/978-1-4612-3364-0_6.

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Chapler, C. K., M. J. Melinyshyn, S. M. Villeneuve, and S. M. Cain. "The Role of Beta-Adrenergic Receptors in the Cardiac Output Response During Carbon Monoxide Hypoxia." In Oxygen Transfer from Atmosphere to Tissues. Springer US, 1988. http://dx.doi.org/10.1007/978-1-4684-5481-9_12.

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Kashkin, Valentine, Roman Odintsov, Tatyana Rubleva, Alexey Romanov, and Konstantin Simonov. "The Lower Atmosphere Response to Seismic Events Using Satellite Data." In Springer Proceedings in Earth and Environmental Sciences. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-31970-0_54.

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Conference papers on the topic "Atmosphere response"

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Schaaf, David A. "Preventing Corrosion Related Electrical Failures: the Response to RoHS." In CORROSION 2014. NACE International, 2014. https://doi.org/10.5006/c2014-4411.

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Abstract Corrosion by definition is the gradual destruction of a material, usually metals, by chemical reaction with its environment. During this reaction, metal is dissolved into an electrolyte, and oxygen from the atmosphere is reduced in the solution. Also, contaminants such as H2S, SO2, Cl2 can often accelerate this reaction. In recent years, the miniaturization of electronic components and the elimination of lead-based solder via restriction of hazardous substances (RoHS) have made the corrosion of electronics a matter of increasing concern. Corrosion causes failures in electronics by cre
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Jaeger, Paul F. "Characterization of Volatile Corrosion Inhibitors Using the Quartz Crystal Microbalance and Supporting Techniques." In CORROSION 1997. NACE International, 1997. https://doi.org/10.5006/c1997-97180.

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Abstract Corrosion inhibitors such as Volatile Corrosion Inhibitors (VCI's) and Contact Corrosion Inhibitors have become loosely ambiguous and differentiating between the two can become a gray area. For example, and the most common mistake is, classifying a material as a VCI when it is a contact inhibitor. Analytical techniques to qualify a material as a VCI have been investigated in order to clarify this ambiguity and to qualify the techniques and equipment for use in the determination of a VCI. The Quartz Crystal Microbalance (QCM) and an atmospheric corrosion monitor were used to characteri
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Sutton, Nathaniel G., Jiang Zhe, Shengxi Li, Hongbo Cong, and Xiaoliang Zhu. "Multiplexed Sensor Array for Accurate Time-of-Wetness (TOW) Measurement." In CORROSION 2017. NACE International, 2017. https://doi.org/10.5006/c2017-09370.

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Abstract Many factors influence atmospheric corrosion, including time-of-wetness (TOW), relative humidity (%RH), structure geometry, contaminant presence, and etc. Current TOW sensor capabilities are limited, measuring galvanic current, electrical resistance, or impedance. Wetness is determined by comparing the sensor output to threshold values that may not relate accurately to corrosion phenomena. In this work, we use electrochemical impedance spectroscopy (EIS) to observe the response of a single interdigital transducer (IDT) sensor to different wetting conditions, including electrolyte volu
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Singh, Harjot, Diego Ochoa, Michael Kloesel, et al. "Corrosion Studies of Novel Nickel-Base Alloys in Molten Chloride Salts." In CONFERENCE 2024. AMPP, 2024. https://doi.org/10.5006/c2024-21199.

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Abstract Molten salts are being considered for use in a new generation of nuclear reactors. Therefore, any materials selection process necessarily involves corrosion studies to understand the compatibility between the salts of interest and the materials of construction. This project investigated the corrosion behavior of novel Ni-base superalloys in molten chloride salt mixtures at 750°C for 200 hours in an inert atmosphere. Alloy response to the molten salt was examined through mass loss per unit area, analysis of surface phases and microstructural examination of the alloy cross-section along
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Duque, Earl, Pankaj Jha, Jessica Bashioum, and Sven Schmitz. "Turbulence Transport Phenomena in the Wakes of Wind Turbines." In Vertical Flight Society 70th Annual Forum & Technology Display. The Vertical Flight Society, 2014. http://dx.doi.org/10.4050/f-0070-2014-9687.

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A true physical understanding of the subtleties involved in the recovery process of the wake momentum deficit downstream of utility-scale wind turbines in the atmosphere has not been obtained to date. While the wind energy community has now a better understanding of some of the effect of the atmospheric stability state on wind turbine power production and wake recovery within an array of wind turbines, available field data are, in general, not acquired at sufficient spatial and temporal resolution that would allow to dissecting some of the mysteries of wake turbulence. It is here that the Actu
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Steakley, Bruce C., Aidan E. Roche, John B. Kumer, Lanny W. Sterritt, Juan C. Dawson, and Charles M. Reilly. "Cryogenic Limb Array Etalon Spectrometer (CLAES) Overview and System Spatial Response Calibration." In Optical Remote Sensing of the Atmosphere. Optica Publishing Group, 1990. http://dx.doi.org/10.1364/orsa.1990.ma6.

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Significant attention is focused on the study of the upper atmosphere and the potential effects of changes in the climate, weather, and protection provided by the ozone layer. The NASA Upper Atmospheric Research Satellite (UARS) (figure 1) , will provide a global, continuous, and comprehensive look at the upper atmosphere over an 18 month period with scheduled launch in the fall of 1991. The Cryogenic Limb Array Etalon Spectrometer (CLAES) will derive Stratospheric temperatures and constituent number densities from the measurement of infrared spectral emissions. Overviews of the CLAES experime
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Herman, B. J., and M. J. Konopnicki. "Response of the atmospheric sodium layer to short optical pulse excitation." In OSA Annual Meeting. Optica Publishing Group, 1991. http://dx.doi.org/10.1364/oam.1991.fr2.

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Some of the adaptive optics systems contemplated to ameliorate the effects of the atmospheric turbulence utilize guide stars. Guide stars are artificial beacons formed in the atmosphere by the interaction of a laser with matter in the atmosphere. Sodium guide stars are formed as a result of laser interaction with the sodium layer in the upper atmosphere. A small rf FEL is one of the candidates considered as a potential source capable of creating a sodium beacon. The pulse format of such a laser consists of trains of short optical pulses. The duration of an individual pulse is typically shorter
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Kirby, Sarah A. V., Edward P. Hamlin, Arthur Y. Hsu, Kathleen M. Kubicek, and Kevin L. Parks. "International Space Station Hazardous Atmosphere Response & amp; Recovery Operations." In International Conference On Environmental Systems. SAE International, 1997. http://dx.doi.org/10.4271/972335.

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Riabova, Svetlana A., Yaroslav O. Romanovsky, and Alexander A. Spivak. "Remote response of electrical characteristics of the atmosphere to strong earthquakes." In 27th International Symposium on Atmospheric and Ocean Optics, Atmospheric Physics, edited by Oleg A. Romanovskii and Gennadii G. Matvienko. SPIE, 2021. http://dx.doi.org/10.1117/12.2602007.

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Gunson, M. R., and C. B. Farmer. "Overview of Atmos Results from Spacelab 3." In Optical Remote Sensing of the Atmosphere. Optica Publishing Group, 1990. http://dx.doi.org/10.1364/orsa.1990.mc2.

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The Atmospheric Trace Molecule Spectroscopy (ATMOS) experiment is an investigation of the distribution of neutral constituents in the earth’s atmosphere. The ATMOS instrument is a Michelson interferometer, with a response to radiation in the near- to mid-infrared, designed to make observations from on board the space shuttle in the solar occultation mode.1,2 Its first flight was made as part of the Spacelab 3 (SL-3) payload which flew on the shuttle "Challenger" between April 29 and May 6, 1989. The ATMOS experiment gathered data during 20 occultation events; 13 sunset occultations located bet
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Reports on the topic "Atmosphere response"

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Green, J., and K. Almenas. Containment atmosphere response to external sprays. Office of Scientific and Technical Information (OSTI), 1995. http://dx.doi.org/10.2172/107787.

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Branch, Brittany, Chad McCoy, and Andrew Vackel. Impact Response of Control Atmosphere Plasma Spray Deposited Materials. Office of Scientific and Technical Information (OSTI), 2022. http://dx.doi.org/10.2172/1868139.

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Zappa, Christopher J. Ocean Surface Temperature Response to Atmosphere-Ocean Interaction of the MJO. Defense Technical Information Center, 2011. http://dx.doi.org/10.21236/ada557074.

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Haaser, Robert A. Understanding the Atmospheric and Ionospheric Response to Bolides and Hypersonic Objects in the Atmosphere (Update Talk, 4/7/2016). Office of Scientific and Technical Information (OSTI), 2016. http://dx.doi.org/10.2172/1250719.

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Coughenour, M. B., T. G. F. Kittel, R. A. Pielke, and J. Eastman. Grassland/atmosphere response to changing climate: Coupling regional and local scales. Final report. Office of Scientific and Technical Information (OSTI), 1993. http://dx.doi.org/10.2172/10104541.

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Stratton, R. A., and A. J. Stirling. Examining the dynamical response to convective heating using an idealised version of the Met Office’s Unified Model. Met Office, 2024. http://dx.doi.org/10.62998/ouao1203.

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In global circulation models, poor coupling between convection parametrizations and the resolved dynamics poses significant obstacles to the representation of a range of convectively coupled atmospheric phenomena. Here we focus on one part of this coupling and ask whether the dynamical response to convection can adequately be captured when convection is parametrized only as heat and moisture sources to the resolved scale, (as is usually the case in convection parametrizations), and without including either mass, or vertical momentum transport terms. To this end, a ‘perfect’ convection parametr
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Wilson, D., Steven Peckham, Max Krackow, Sora Haley, Sophia Bragdon, and Jay Clausen. Discriminating buried munitions based on physical models for their thermal response. Engineer Research and Development Center (U.S.), 2025. https://doi.org/10.21079/11681/49749.

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Munitions and other objects buried near the Earth’s surface can often be recognized in infrared imagery because their thermal and radiative properties differ from the surrounding undisturbed soil. However, the evolution of the thermal signature over time is subject to many complex interacting processes, including incident solar radiation, heat conduction in the ground, longwave radiation from the surface, and sensible and latent heat exchanges with the atmosphere. This complexity makes development of robust classification algorithms particularly challenging. Machine-learning algorithms, althou
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Wilson, D., Michael Shaw, Vladimir Ostashev, et al. Numerical modeling of mesoscale infrasound propagation in the Arctic. Engineer Research and Development Center (U.S.), 2022. http://dx.doi.org/10.21079/11681/45788.

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The impacts of characteristic weather events and seasonal patterns on infrasound propagation in the Arctic region are simulated numerically. The methodology utilizes wide-angle parabolic equation methods for a windy atmosphere with inputs provided by radiosonde observations and a high-resolution reanalysis of Arctic weather. The calculations involve horizontal distances up to 200 km for which interactions with the troposphere and lower stratosphere dominate. Among the events examined are two sudden stratospheric warmings, which are found to weaken upward refraction by temperature gradients whi
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Fitzpatrick, Patrick, and Yee Lau. CONCORDE Meteorological Analysis (CMA) - Data Guide. The University of Southern Mississippi, 2023. http://dx.doi.org/10.18785/sose.003.

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CONCORDE is the CONsortium for oil spill exposure pathways in COastal River-Dominated Ecosystems (CONCORDE), and is an interdisciplinary research program funded by the Gulf of Mexico Research Initiative (GoMRI) to conduct scientific studies of the impacts of oil, dispersed oil and dispersant on the Gulf’s ecosystem (Greer et al. 2018). A CONCORDE goal is to implement a synthesis model containing circulation and biogeochemistry components of the Northern Gulf of Mexico shelf system which can ultimately aid in prediction of oil spill transport and impacts. The CONCORDE Meteorological Analysis (C
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Zappa, Christopher J. Ocean Surface Temperature Response to Atmosphere-Ocean Interaction of the MJO: A Component of Coupled Air-Wave-Sea Processes in the Subtropics Department Research Initiative. Defense Technical Information Center, 2012. http://dx.doi.org/10.21236/ada572583.

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