Academic literature on the topic 'Earth interactions'
Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles
Consult the lists of relevant articles, books, theses, conference reports, and other scholarly sources on the topic 'Earth interactions.'
Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.
You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.
Journal articles on the topic "Earth interactions"
Orcutt, J., and J. Holoviak. "Earth Interactions: A new journal." Eos, Transactions American Geophysical Union 76, no. 20 (1995): 201. http://dx.doi.org/10.1029/95eo00117.
Full textRycroft, M. J. "The aurora: Sun-Earth interactions." Journal of Atmospheric and Solar-Terrestrial Physics 59, no. 11 (July 1997): 1359. http://dx.doi.org/10.1016/s1364-6826(97)88690-7.
Full textAnonymous. "Earth Interactions now inviting submissions." Eos, Transactions American Geophysical Union 76, no. 48 (1995): 490. http://dx.doi.org/10.1029/95eo00303.
Full textGadsden, M. "The aurora: Sun-earth interactions." Journal of Atmospheric and Terrestrial Physics 55, no. 9 (July 1993): 1314. http://dx.doi.org/10.1016/0021-9169(93)90061-3.
Full textChin, Anne, Rong Fu, Jon Harbor, Mark P. Taylor, and Veerle Vanacker. "Anthropocene: Human interactions with earth systems." Anthropocene 1 (September 2013): 1–2. http://dx.doi.org/10.1016/j.ancene.2013.10.001.
Full textKasuya, T. "Exchange interactions in rare earth compounds." Journal of Alloys and Compounds 192, no. 1-2 (February 1993): 11–16. http://dx.doi.org/10.1016/0925-8388(93)90171-i.
Full textKadomtseva, A. M., A. K. Zvezdin, A. P. Pyatakov, A. V. Kuvardin, G. P. Vorob’ev, Yu F. Popov, and L. N. Bezmaternykh. "Magnetoelectric interactions in rare-earth ferroborates." Journal of Experimental and Theoretical Physics 105, no. 1 (July 2007): 116–19. http://dx.doi.org/10.1134/s1063776107070254.
Full textSimpson, Joanne, and Keith Seitter. "Earth Interactions: A New Electronic Journal." Bulletin of the American Meteorological Society 76, no. 5 (May 1, 1995): 653–54. http://dx.doi.org/10.1175/1520-0477-76.5.653.
Full textSellers, Piers, and James J. McCarthy. "Planet Earth: Part III: Biosphere interactions." Eos, Transactions American Geophysical Union 71, no. 52 (1990): 1883. http://dx.doi.org/10.1029/90eo00383.
Full textBenelli, Cristiano, Andrea Caneschi, Dante Gatteschi, and Luca Pardi. "Magnetic interactions involving rare earth ions." Materials Chemistry and Physics 31, no. 1-2 (March 1992): 17–22. http://dx.doi.org/10.1016/0254-0584(92)90147-z.
Full textDissertations / Theses on the topic "Earth interactions"
Mukherjee, Rick. "Strong interactions in alkaline-earth Rydberg ensembles." Doctoral thesis, Saechsische Landesbibliothek- Staats- und Universitaetsbibliothek Dresden, 2014. http://nbn-resolving.de/urn:nbn:de:bsz:14-qucosa-157228.
Full textGhan, S. J. (Steven John). "Unstable radiative-dynamical interactions." Thesis, Massachusetts Institute of Technology, 1988. http://hdl.handle.net/1721.1/52897.
Full textGoodman, Jason (Jason Curtis) 1973. "Interannual middle-latitude atmosphere-ocean interactions." Thesis, Massachusetts Institute of Technology, 2001. http://hdl.handle.net/1721.1/16779.
Full textIncludes bibliographical references (p. 144-151).
This electronic version was submitted by the student author. The certified thesis is available in the Institute Archives and Special Collections.
This thesis discusses the interaction of atmosphere and ocean in midlatitudes on interannual and decadal timescales. We investigate the extent to which mutuallycoupled atmosphere-ocean feedback can explain the observed coupled variability on these timescales, and look for preferred modes of atmospheric response to forcing by sea-surface temperature anomalies. First, we formulate and study a very simple analytical model of the mutual interaction of the middle-latitude atmosphere and ocean. The model is found to support coupled modes in which oceanic baroclinic Rossby waves of decadal period grow through positive coupled feedback between the thermal forcing of the atmosphere induced by associated SST anomalies and the resulting windstress forcing of the ocean. Growth only occurs if the atmospheric response to thermal forcing is equivalent barotropic, with a particular phase relationship with the underlying SST anomalies. The dependence of the growth rate and structure of the modes on the nature of the assumed physics of air-sea interaction is explored, and their possible relation to observed phenomena discussed. We then construct a numerical model with the same physics; this enables us to consider the effects of nontrivial boundary conditions and background flows within the model. We find that the finite fetch of a closed ocean basin reduces growth rate and can lead to decay. However, the coupled mode described above remains the least-damped, and is thus the pattern most easily energized by stochastic forcing. Using a non-uniform atmospheric background flow focuses perturbation energy into particular areas, so that the coupled mode's expression in the atmosphere becomes fixed in space, rather than propagating. This improves the mode's resemblance to observed patterns of variability, such as the North Atlantic Oscillation, which are generally stationary patterns which fluctuate in intensity. The atmospheric component of the coupled mode exists in a balance between Rossby-wave propagation and vorticity advection. This is the same balance as the "neutral vectors" described by Marshall and Molteni (1993). Neutral vectors are the right singular vectors of the linearized atmospheric model's tendency matrix that have the smallest eigenvalues; they are also the patterns that exhibit the largest response to forcing perturbations in the linear model. We explain how the coupled mode arises as the ocean excites atmospheric neutral vectors. Neutral vectors act as pattern-specific amplifiers of ocean SST anomalies. We then proceed to study the neutral vectors of a quasigeostrophic model with realistic mean flow. We find a striking similarity between these patterns and the dominant patterns of variability observed in both the full nonlinear model and in the real world. We provide a mathematical explanation for this connection. Investigation of the "optimal forcing patterns" - the left singular vectors - proves to be less fruitful. The neutral modes have equivalent barotropic vertical structure, but their optimal forcing patterns are baroclinic and seem to be associated with low level heating. But the horizontal patterns of the forcing patterns are not robust, and are sensitive to the form of the inner product used in the SVD analysis. Additionally, applying "optimal" forcing patterns as perturbations to the full nonlinear model does not generate the response suggested by the linear model.
by Jason Goodman.
Ph.D.
Straub, Kyle M. "Quantifying turbidity current interactions with topography." Thesis, Massachusetts Institute of Technology, 2007. http://hdl.handle.net/1721.1/40864.
Full textThis electronic version was submitted by the student author. The certified thesis is available in the Institute Archives and Special Collections.
Includes bibliographical references (p. 196-205).
This thesis advances our understanding of how transport properties of turbidity currents are mediated by interactions with seafloor topography, specifically channelized surfaces. Turbidity currents are responsible for crafting the morphology of continental margins. Unfortunately, very few direct observations exists defining turbidity current interactions with submarine channels and canyons because infrequent occurrence, great water depths, and high current velocities make measurements difficult to obtain. To overcome this problem, I utilize reduced scale laboratory experiments, remote sensing of the seafloor and subsurface deposits, and numerical analysis of transport processes. I focus on resolving the topography and composition of the evolving water-sediment interface with additional measurements that characterize the sediment transport and flow fields. I begin by quantifying interactions between turbidity currents and channel-bounding levees. Levees are the primary elements of self-formed channels and act to confine flows within channels, thereby increasing transport efficiency. I quantify the morphology and growth of levees in a submarine channel network offshore Borneo. Levee deposit trends are interpreted using laboratory observations and a morphodynamic model describing levee growth. Channel and levee deposits resulting from interactions between turbidity currents and sinuous submarine channels are then studied using reduced-scale laboratory experiments. Measurements of current superelevation in channel bends are used to illustrate the importance of current runup onto the outer banks of channel bends. This runup resulted in focused overbank flow and production of thick, coarse, steep levees at these sites.
(cont.) Additional laboratory experiments illustrate the importance of current-channel bend interactions to the runout length of turbidity currents. I observed enhanced mixing in channel bends that reduced proximal deposition rates in sinuous channels compared to straight channels. I hypothesize that a wholesale vertical mixing of suspended sediment within turbidity currents at channel bends is a necessary condition for the construction of submarine channels greater than 100 km in length. Finally, I document the deepening of submarine canyons under net depositional conditions using an industry-grade seismic volume from the continental slope offshore Borneo. Interpretation of seismic horizons suggests deposition resulted from sheet-like turbidity currents, highlighting the importance of unconfined currents to the evolution of seascapes.
by Kyle M. Straub.
Ph.D.
Shah, N. J. "Hyperfine interactions in amorphous and crystalline alloys containing rare earth metals." Thesis, University of Manchester, 1987. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.377743.
Full textMenon, Surabi. "Role of Sulfates in Regional Cloud-Climate Interactions." NCSU, 1998. http://www.lib.ncsu.edu/theses/available/etd-19981102-133647.
Full textAerosols affect the radiation budget of the earth-atmosphere system by directly reflecting or absorbing solar radiation and also indirectly, by altering the cloud albedo through changes in the cloud condensation nuclei concentration (CCN). Increases in CCN concentrations result in an increase in the cloud droplet number concentration (N). Assuming the cloud liquid water content (LWC) stays the same, this will result in smaller cloud droplet sizes. Thus, this will increase cloud reflectance and cloud lifetime as cloud cover also increases. An accurate quantification of the aerosol forcing effect is still not possible due to the complexity involved in understanding aerosol processes and their effects on climate. There has also been a lack of a coordinated effort toward linking surface and in situ observations, as well climate model results and satellite data. Due to the spatial and temporal heterogeneity in aerosol forcing, regional effects are important. In this dissertation, the direct and indirect radiative forcing effects of aerosols - primarily sulfates and to lesser extent soot aerosols at a site located in the southeastern U.S. are investigated by means of surface observations, modeling results and satellite data.During the summers of 1993-96, field experiments were conducted at Mt. Mitchell, North Carolina, at a site representative of the southeastern U.S. to determine the effect of pollutants on the cloud microphysical and optical properties. Analyses of the results from empirical relationships are used to obtain an estimate of the contribution of sulfates to indirect radiative forcing. Concurrent measurements of size resolved chemical concentrations, light scattering and absorption coefficients, aerosol size distribution and optical depth measurements were obtained during the winter of 1997 for cloud-free skies. Data from these measurements are used to investigate the chemical-physical-optical interaction between aerosols and to determine the direct forcing effect of aerosols by means of a column forcing model. Cloud water sulfate concentration is used as a measure of anthropogenic pollution. Back-trajectory analysis is used to identify the source of the air masses classified as polluted continental, continental and marine. The effect of anthropogenic pollution on cloud microphysical properties such as LWC, N, effective radii (Reff), CCN activation spectrum, cloud optical depth and reflectivity are investigated. The relationship between Reff and sulfate for different air masses, as well as the N-sulfate mass relationship, suggests that the counteracting effect of sulfates on greenhouse warming for the southeastern U.S. would be of a magnitude greater than -4.0 W m-2 obtained by previous modeling studies. Acidity variations between cloud droplets of different sizes indicated that on an average, smaller drops are enriched in sulfates, nitrates and ammonium, whereas, larger droplets have higher concentrations of sodium, calcium and magnesium. As part of a closure experiment cloud albedo calculated from in situ measurements was compared to that retrieved from the Advanced Very High Resolution Radiometer data for four years (1993-96). The nonlinear relationships between the cloud microphysical/optical properties and the sulfate content imply the existence of an optimum level for the sulfate concentration that would affect cloud albedo. In terms of the direct forcing effect, wintertime forcing obtained for an internal mixture of sulfate and soot aerosols is much lower than that obtained during summer, due to reduced sulfate concentrations in winter. A quantitative measure of the direct forcing indicates higher magnitudes both for summer and winter than is obtained from previous modeling results. Analyses of the direct and indirect radiative forcing effect of sulfates for the southeastern U.S. indicate that the negative forcing effect is of greater magnitude than is predicted by modeling results. Thus, reduction in sulfate emissions would have a significant impact on climate for the southeastern U.S.
McMorrow, D. F. "Crystal fields and hyperfine interactions in holmium compounds." Thesis, University of Manchester, 1987. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.377728.
Full textJerry, Ruel (Ruel Valentine). "Effects of subsurface fracture interactions on surface deformation." Thesis, Massachusetts Institute of Technology, 2013. http://hdl.handle.net/1721.1/84911.
Full textCataloged from PDF version of thesis.
Includes bibliographical references (pages 63-64).
Although the surface deformation resulting from the opening of a single fracture in a layered elastic half-space resembles the observed deformation at the InSalah site, it seems unlikely that only a single fracture is involved. This raises the question of how interaction among multiple fractures affects surface deformation. Finite element modeling is used to build a 3D model of a reservoir with multiple fractures. The interacting cracks and fractures give this model a more complicated stress state, and so any surface deformation would be different from that of a model with a single fracture. Geodetic monitoring of large-scale CO 2 sequestration provides a potentially powerful and cost-effective tool for interrogating reservoir structure and processes. For example, InSAR observations at the InSalah, Algeria sequestration site have mapped the surface deformation above an active reservoir, and helped delineate the effects of CO2 storage. The impact of interactions on individual fractures and the qualitative changes in the surface displacement and stress fields are considered and the importance of orientation, position and fracture area is investigated. It was found that when the crack locations are biased towards stacked parallel arrangements, then the shielding effect of interactions dominates, meaning that the overall stiffness of a representative volume increases. When collinear interactions dominate then the overall stiffness is reduced. These effects are then used to find a volume average and a continuum description of a solid with effective elastic properties. In this way a volume of fractured rock can be replaced with a representative volume with elastic properties that approximate the interaction effects.
by Ruel Jerry.
S.M.in Geophysics
Moore, Kelsey Reed. "Cyanobacterial evolution and interactions with the Proterozoic world." Thesis, Massachusetts Institute of Technology, 2020. https://hdl.handle.net/1721.1/127144.
Full textCataloged from the official PDF of thesis.
Includes bibliographical references.
Our understanding of the biosphere prior to the rise of complex life is built largely upon microbial mat structures and some exceptionally well-preserved microbial fossils from the Proterozoic (2500 to 540 million years ago). Some of these exceptional fossils are identifiable as cyanobacteria that were preserved by pyrite, amorphous silica (SiO₂) and other minerals. Although a record exists of these organisms, the sparse nature of fossil assemblages and simplicity of many Proterozoic fossil morphologies makes it difficult to identify specific taxa or create a complete picture of the ancient biosphere and how it interacted with the early Earth. Cyanobacteria are thought to have evolved early in Earth history and played a large part in shaping the ancient biosphere and geosphere, but questions remain about their evolution and the ways in which cyanobacterial communities interacted with the Earth during the Proterozoic Eon.
In this thesis, I seek to build a more complete understanding the record of Proterozoic cyanobacteria, their responses to environmental perturbations and the chemical conditions and microbe-mineral interactions that characterized the Proterozoic marine realm. I begin by investigating the evolutionary relationships between different cyanobacterial lineages and their relationship to chloroplasts. I then analyze an assemblage of pyritized cyanobacteria that were preserved during the Cryogenian and provide a record of primary productivity in the oceans following a global glaciation. Finally, I investigate factors that enabled the fossilization of some exceptionally preserved cyanobacteria and implications of these mechanisms for cyanobacterial biochemistry, chemical conditions, and interactions between microbes and Proterozoic tidal environments.
The combined molecular, fossil and experimental insights allow us to go beyond morphological interpretations of microbial fossils and build a more complete understanding of the evolutionary history of cyanobacteria, the types of cyanobacteria that were preserved during the Proterozoic, the responses of these cyanobacteria to environmental stresses and the interactions of those cyanobacteria with the evolving seawater chemistry.
by Kelsey R. Moore.
Ph. D.
Ph.D. Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences
Gunturu, Udaya Bhaskar. "Aerosol-Cloud interactions : a new perspective in precipitation enhancement." Thesis, Massachusetts Institute of Technology, 2010. http://hdl.handle.net/1721.1/58462.
Full textCataloged from PDF version of thesis.
Includes bibliographical references (p. 171-184).
Increased industrialization and human activity modified the atmospheric aerosol composition and size-distribution during the last several decades. This has affected the structure and evolution of clouds, and precipitation from them. The processes and mechanisms by which clouds and precipitation are modified by changes in aerosol composition and size-distribution are very intricate. The objective of this thesis is to improve the understanding of the processes and mechanisms through which the changes in aerosol concentrations impact the evolution of deep convective clouds and precipitation formation. We develop a new coupled model in which a very detailed model of aerosol activation is coupled to a three-dimensional cloud resolving model. This coupled model can accurately represent different kinds of aerosol populations. This coupled model is used to investigate the impact of changing aerosol concentrations on the dynamics, microphysical evolution and precipitation formation in deep convective clouds. We examine the theories of aerosol activation, and the representation of aerosol activation in cloud models. The limitations of the extant methods of representation of aerosol activation in cloud models are evaluated. Then we descibe the components of the coupled model - Modified Eulerian and Lagrangian Aerosol Model (MELAM) and the Cloud Resolving Model (CRM). The features of these two component models with respect to aersol activation and cloud formation are discussed. The evaluation of the coupled model by simulation of a deep convertive event observed during the INDian Ocean EXperiment (INDOEX) by statistcal comparison of observed and simulated cloud fields shows that the coupled model can simulate deep convective events reasonably well. We present a study of the senstivity of the model to initial thermodynamic conditions (CAPE). Different initial thermodynamic conditons sampled during the INDOEX are used to initialize the coupled model and, the structure and evolution of the deep convective event are discussed. The study sheds new light on the respone of deep convection to CAPE. It is found that when the atmosphere has moderate CAPE, the precipitation forming processes are very active and when the CAPE is (cont.) low or high, they are comparatively less efficient.
As the most important part of our study, we examine the response of deep convection to changing initial aerosol concentration. Different aerosol concentrations from those representing pristine to polluted atmospheres are considered. We look at the buoyancy of the cloud and the microphysical evolution. It is found that the dynamics and microphysics are tightly coupled and we infer that to understand aerosol-cloud interactions in deep convective clouds, both - dynamics and microphysics - and their interaction have to be taken into consideration. Our results show that the response of a deep convective cloud to changing aerosol concentration is very different from the much well understood reponse of shallow clouds or small cumulus clouds. In general, increase in aerosol concentratin is seen to invigorate convection and lead to greater condensate. Although the cloud droplet size decreases, collision-coalescence is not completely inefficient. The precipitation in high aerosol regime is seen to occure in short spells of intense rain. A very interesting anomalous response of deep convection to initial aerosol concentration is observed at intermediate aerosol concentrations. The cloud lifetime, and precipitation are seen to increase in this regime. A possible mechanism to explain this anomalous behavior is proposed and the available circumstantial support for the mechanism from extant observations is presented. It is proposed that the efficient collection of rain and cloud droplets by ice and graupel particles in the middle troposphere is primarily responsible for this increased cloud lifetime and precipitation.
by Udaya Bhaskar Gunturu.
Ph.D.
Books on the topic "Earth interactions"
Bone, Neil. The aurora: Sun-earth interactions. 2nd ed. Chichester: Wiley, 1996.
Find full textThe aurora: Sun-earth interactions. New York: E. Horwood, 1991.
Find full textAxel, Liebscher, and Heinrich Christoph A. 1953-, eds. Fluid-fluid interactions. Chantilly, Va: Mineralogical Society of America, Geochemical Society, 2007.
Find full textMiller, E. Willard. Physical geography: Earth systems and human interactions. Columbus: C.E. Merrill, 1985.
Find full textEckart, Ehlers, and Krafft Thomas, eds. Understanding the earth system: Compartments, processes, and interactions. Berlin: Springer, 2001.
Find full textW, Avakian Robert, ed. Science interactions. New York: Glencoe/McGraw-Hill, 1999.
Find full textThomas H. Kean New Jersey State Aquarium. The Ocean: Exploring interactions beneath the waves. New York: Scholastic, 1997.
Find full textPandey, Dhananjai K., M. Ravichandran, and Nisha Nair, eds. Dynamics of the Earth System: Evolution, Processes and Interactions. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-40659-2.
Full textLi, Yagang. Hy perfine interactions in the rare earth intermetallic compounds. Manchester: University of Manchester, 1994.
Find full textJeng, Dong-Sheng. Porous Models for Wave-seabed Interactions. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013.
Find full textBook chapters on the topic "Earth interactions"
Harrison, T. Mark. "Plate Boundary Interactions Through Geologic History." In Hadean Earth, 123–42. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-46687-9_6.
Full textResco de Dios, Víctor. "Fire as an Earth System Process." In Plant-Fire Interactions, 31–51. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-41192-3_3.
Full textTuffen, Hugh. "Ice-Volcano Interactions." In Encyclopedia of Earth Sciences Series, 625–28. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2642-2_289.
Full textEymard, Laurence, and Gilles Reverdin. "Ocean-Atmosphere Interactions." In Ocean in the Earth System, 105–44. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2014. http://dx.doi.org/10.1002/9781119007678.ch3.
Full textVihma, Timo. "Atmosphere-Snow/Ice Interactions." In Encyclopedia of Earth Sciences Series, 66–75. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2642-2_31.
Full textSmith, Sharon L., and Margo M. Burgess. "Permafrost and Climate Interactions." In Encyclopedia of Earth Sciences Series, 852–57. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2642-2_401.
Full textKruse-Graumann, Lenelis. "Commentary on “Modelling Human Interactions with the Environment”." In Earth System Analysis, 488–89. Berlin, Heidelberg: Springer Berlin Heidelberg, 1998. http://dx.doi.org/10.1007/978-3-642-52354-0_27.
Full textMohr, Tillmann. "Commentary on “Modelling Human Interactions with the Environment”." In Earth System Analysis, 490–91. Berlin, Heidelberg: Springer Berlin Heidelberg, 1998. http://dx.doi.org/10.1007/978-3-642-52354-0_28.
Full textKrishna, K. S., and M. Ismaiel. "Mantle Plume – Spreading Ridge Interactions." In Encyclopedia of Solid Earth Geophysics, 1–10. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-10475-7_262-1.
Full textKrishna, K. S., and M. Ismaiel. "Mantle Plume: Spreading Ridge Interactions." In Encyclopedia of Solid Earth Geophysics, 1085–94. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-58631-7_262.
Full textConference papers on the topic "Earth interactions"
Anz-Meador, Phillip D. "Tether-debris interactions in low Earth orbit." In Space technology and applications international forum - 2001. AIP, 2001. http://dx.doi.org/10.1063/1.1357972.
Full textMoe, Kenneth, and Mildred M. Moe. "Gas-Surface Interactions in Low-Earth Orbit." In 27TH INTERNATIONAL SYMPOSIUM ON RAREFIED GAS DYNAMICS. AIP, 2011. http://dx.doi.org/10.1063/1.3562825.
Full textDreyer, C. B., and A. Abbud-Madrid. "Laboratory Studies of Physical Interactions of Exploration Hardware with Surfaces of Airless Bodies." In Earth and Space 2014. Reston, VA: American Society of Civil Engineers, 2015. http://dx.doi.org/10.1061/9780784479179.013.
Full textSissmann, O., P. Bachaud, T. Parra, M. Chardin, and M. Masson. "Experimental and Numerical Study of CO2-water-minerals Interactions Applied to Rousse Reservoir Rock." In Sustainable Earth Sciences 2013. Netherlands: EAGE Publications BV, 2013. http://dx.doi.org/10.3997/2214-4609.20131589.
Full textBaker, Daniel N. "Wave-Particle Interactions in Earth Outer Radiation Zone." In 2022 International Conference on Electromagnetics in Advanced Applications (ICEAA). IEEE, 2022. http://dx.doi.org/10.1109/iceaa49419.2022.9899981.
Full textBanks, Bruce, Sharon Miller, and Kim de Groh. "Low Earth Orbital Atomic Oxygen Interactions with Materials." In 2nd International Energy Conversion Engineering Conference. Reston, Virigina: American Institute of Aeronautics and Astronautics, 2004. http://dx.doi.org/10.2514/6.2004-5638.
Full textRemo, John L., and Peter X. Hammerling. "High energy density interactions for near-earth orbit perturbations." In High-Power Laser Ablation 2004, edited by Claude R. Phipps. SPIE, 2004. http://dx.doi.org/10.1117/12.547674.
Full textLabandibar, Jean-Yves, Franck Jubineau, Pierluigi Silvestrin, and Umberto Del Bello. "ESA Earth Explorer Land Surface Processes and Interactions mission." In SPIE's International Symposium on Optical Science, Engineering, and Instrumentation, edited by Michael R. Descour and Sylvia S. Shen. SPIE, 1999. http://dx.doi.org/10.1117/12.366277.
Full textLabandibar, Jean-Yves, Franck Jubineau, Pierluigi Silvestrin, and Umberto Del Bello. "The esa earth explorer land surface processes and interactions mission." In International Conference on Space Optics 2000, edited by Georges Otrio. SPIE, 2017. http://dx.doi.org/10.1117/12.2307901.
Full textStephani, Kelly A., and Iain D. Boyd. "Dynamics of Spacecraft Plume/Magnetosphere Interactions in Geostationary Earth Orbit." In 53rd AIAA Aerospace Sciences Meeting. Reston, Virginia: American Institute of Aeronautics and Astronautics, 2015. http://dx.doi.org/10.2514/6.2015-1396.
Full textReports on the topic "Earth interactions"
Minton, Timothy K. Space Vehicle Material and Plume Interactions With the Low Earth Orbital Environment. Fort Belvoir, VA: Defense Technical Information Center, January 2008. http://dx.doi.org/10.21236/ada476326.
Full textMa, Po-Lun, Christopher Bretherton, Panos Stinis, Vince Larson, Elizabeth Barnes, Sam Silva, Joseph Hardin, et al. Facilitating better and faster simulations of aerosol-cloud interactions in Earth system models. Office of Scientific and Technical Information (OSTI), April 2021. http://dx.doi.org/10.2172/1769709.
Full textPerdigão, Rui A. P. Earth System Dynamic Intelligence - ESDI. Meteoceanics, April 2021. http://dx.doi.org/10.46337/esdi.210414.
Full textKim, Grace, Stefanie Mack, and Daniel Kaufman. Combining artificial intelligence, Earth observations, and climate models to improve predictability of ice-biogeochemistry interactions. Office of Scientific and Technical Information (OSTI), April 2021. http://dx.doi.org/10.2172/1769689.
Full textLiu, Xiaohong, and Zhien Wang. Improving Predictability of Mixed-Phase Clouds and Aerosol Interactions in the Community Earth System Model (CESM) with ARM Measurements. Office of Scientific and Technical Information (OSTI), February 2020. http://dx.doi.org/10.2172/1601142.
Full textAsay-Davis, Xylar Storm. Final Report: Modeling coupled ice sheet-ocean interactions in the Model for Prediction Across Scales (MPAS) and in DOE Earth System Models. Office of Scientific and Technical Information (OSTI), January 2019. http://dx.doi.org/10.2172/1490084.
Full textFung, Inez. Final Technical Report for Department of Energy Award DE-SC0010857, “Towards parameterization of root-rock hydrologic interactions in the Earth System Model”. Office of Scientific and Technical Information (OSTI), December 2016. http://dx.doi.org/10.2172/1334372.
Full textHostetler, Steven, Cathy Whitlock, Bryan Shuman, David Liefert, Charles Wolf Drimal, and Scott Bischke. Greater Yellowstone climate assessment: past, present, and future climate change in greater Yellowstone watersheds. Montana State University, June 2021. http://dx.doi.org/10.15788/gyca2021.
Full textVelinov, Peter I. Y., Yordan Tassev, and Dimitrinka Tomova. Study of Unpredicted First Geomagnetic Storm of 2020, Due to Interaction of ICME with Near-earth Space on Аpril 20. "Prof. Marin Drinov" Publishing House of Bulgarian Academy of Sciences, November 2020. http://dx.doi.org/10.7546/crabs.2020.11.12.
Full textEbeling, Robert, and Barry White. Load and resistance factors for earth retaining, reinforced concrete hydraulic structures based on a reliability index (β) derived from the Probability of Unsatisfactory Performance (PUP) : phase 2 study. Engineer Research and Development Center (U.S.), March 2021. http://dx.doi.org/10.21079/11681/39881.
Full text