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Journal articles on the topic 'Atmospheric control'

Author: Grafiati

Published: 4 June 2021

Last updated: 3 February 2022

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1

Kucera, V. "Reduction of air pollutants - a tool for control of atmospheric corrosion." Revista de Metalurgia 39, Extra (2003): 55–61. http://dx.doi.org/10.3989/revmetalm.2003.v39.iextra.1097.

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2

Grzyb, Marta, and Konrad Stefański. "The control of anti-aircraft missile flight path in atmospheric disturbances." Zeszyty Naukowe Akademii Marynarki Wojennej, no. 2 (June 30, 2017): 51–60. http://dx.doi.org/10.5604/01.3001.0010.4066.

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The control of homing surface-to-air short-range anti-aircraft missile takes place in the atmosphere, in which there are different types of atmospheric disturbances such as: turbulence, gust and wind shear. The atmospheric disturbances is generated with the Dryden power spectral density model. This paper presents a method for control of flying objects such as anti-aircraft missile moving in a disturbed environment. The method of proportional navigation will be applied for the guidance of missile on the ground target. The research will include the analysis of influence of atmospherics on the hi

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3

Nisbet, Euan. "Emissions control needs atmospheric verification." Nature 433, no. 7027 (2005): 683. http://dx.doi.org/10.1038/433683b.

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4

Goreau, Thomas J. "Control of atmospheric carbon dioxide." Global Environmental Change 2, no. 1 (1992): 5–11. http://dx.doi.org/10.1016/0959-3780(92)90031-2.

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5

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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6

PASTER, NACHMAN, RIVKA BARKAI-GOLAN, and MOSHE CALDERON. "Control of T-2 Toxin Production Using Atmospheric Gases1." Journal of Food Protection 49, no. 8 (1986): 615–17. http://dx.doi.org/10.4315/0362-028x-49.8.615.

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When the fungus Fusarium tricinctum NRRL 3299 was grown under atmospheres enriched with 50% CO2 and above (given in combination with 20% O2), T-2 production was reduced to 4.0 μg/45 ml of medium, as compared with 21.2 μg/45 ml of medium produced in an atmosphere of air. At 60% CO2/20% O2 and 80% CO2/20% O2, a significant reduction in fungal growth was also observed. The possibility of using controlled atmospheres as a means for mycotoxin control is discussed.

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7

Kim, Dongmin, Sang-Ki Lee, Hosmay Lopez, and Marlos Goes. "Pacific Mean-State Control of Atlantic Multidecadal Oscillation–El Niño Relationship." Journal of Climate 33, no. 10 (2020): 4273–91. http://dx.doi.org/10.1175/jcli-d-19-0398.1.

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AbstractWe investigate the potential impacts of the interdecadal Pacific oscillation (IPO) and Atlantic multidecadal oscillation (AMO) on El Niño and the associated atmosphere and ocean dynamics by using the Community Earth System Model–Large Ensemble Simulation (CESM-LENS). The individual effects of IPO and AMO on El Niño frequency and the underlying atmosphere–ocean processes are well reproduced in CESM-LENS and agree with previous studies. However, the sensitivity of El Niño frequency to the AMO is robust mainly during the negative IPO phase and very weak during the positive IPO phase. Furt

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8

Genchev, G., Cr Hristov, Hr Shehtov, Em Pantev, and S. Georgieva. "Computer Control of Intensive Atmospheric Drying." IFAC Proceedings Volumes 19, no. 12 (1986): 173–79. http://dx.doi.org/10.1016/s1474-6670(17)59610-x.

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9

BAUM, RUDY. "Phytoplankton seen as atmospheric CO control." Chemical & Engineering News 68, no. 22 (1990): 7. http://dx.doi.org/10.1021/cen-v068n022.p007.

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10

Czaja, Arnaud. "Atmospheric Control on the Thermohaline Circulation." Journal of Physical Oceanography 39, no. 1 (2009): 234–47. http://dx.doi.org/10.1175/2008jpo3897.1.

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Abstract In an attempt to elucidate the role of atmospheric and oceanic processes in setting a vigorous ocean overturning circulation in the North Atlantic but not in the North Pacific, a comparison of the observed atmospheric circulation and net surface freshwater fluxes over the North Atlantic and Pacific basins is conducted. It is proposed that the more erratic meridional displacements of the atmospheric jet stream over the North Atlantic sector is instrumental in maintaining high surface salinities in its subpolar gyre. In addition, it is suggested that the spatial pattern of the net fresh

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11

Hogg, Andrew Mc C., William K. Dewar, Peter D. Killworth, and Jeffrey R. Blundell. "Decadal Variability of the Midlatitude Climate System Driven by the Ocean Circulation." Journal of Climate 19, no. 7 (2006): 1149–66. http://dx.doi.org/10.1175/jcli3651.1.

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Abstract A midlatitude coupled ocean–atmosphere model is used to investigate interactions between the atmosphere and the wind-driven ocean circulation. This model uses idealized geometry, yet rich and complicated dynamic flow regimes arise in the ocean due to the explicit simulation of geostrophic turbulence. An interdecadal mode of intrinsic ocean variability is found, and this mode projects onto existing atmospheric modes of variability, thereby controlling the time scale of the atmospheric modes. It is also shown that ocean circulation controls the time scale of the SST response to wind for

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12

Kim, Young-Joon, William F. Campbell, and Steven D. Swadley. "Reduction of Middle-Atmospheric Forecast Bias through Improvement in Satellite Radiance Quality Control." Weather and Forecasting 25, no. 2 (2010): 681–700. http://dx.doi.org/10.1175/2009waf2222329.1.

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Abstract This article discusses a practical problem faced in operational atmospheric forecasting and data assimilation, and efforts to improve forecast quality through the choice of quality control parameters. The need to utilize as much data as possible must be carefully balanced against the need to reject observations deemed erroneous because they are far from the background value. Alleviation of forecast bias in the middle atmosphere for a global atmospheric prediction system is attempted via improvement of the quality control and bias correction of the satellite radiance data; in particula

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13

Wszelaki, Annette L., and Elizabeth J. Mitcham. "411 Elevated Oxygen Atmospheres as a Decay Control Alternative on Strawberry." HortScience 34, no. 3 (1999): 514F—515. http://dx.doi.org/10.21273/hortsci.34.3.514f.

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Controlled atmospheres have been proven an effective postharvest disease deterrent for strawberries both in transport and storage. However, these treatments do not provide residual protection once the commodity is removed from the atmosphere, and the atmospheres can cause off-flavors in the fruit. Elevated oxygen atmospheres are a novel addition to this technology and could potentially provide better decay control without the harmful effects on fruit flavor aspects. Elevated oxygen will potentially discourage microbial growth, as anaerobes grow best under very low oxygen levels and aerobes gro

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14

Somavilla, Raquel, Carmen Rodriguez, Alicia Lavín, Amaia Viloria, Elena Marcos, and Daniel Cano. "Atmospheric Control of Deep Chlorophyll Maximum Development." Geosciences 9, no. 4 (2019): 178. http://dx.doi.org/10.3390/geosciences9040178.

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The evolution of the near-surface phytoplankton bloom towards a Deep Chlorophyll Maximum (DCM) in mid-latitudes and subpolar regions of the global ocean is a well-known biological feature. However, our knowledge about the exact mechanism that determines the end of the bloom and its irreversible evolution towards a DCM is still limited. In this work, combining satellite and in-situ oceanographic data together with reanalysis data, we investigate why and when this transition between the near-surface phytoplankton bloom and the development of a DCM occurs. For this aim, we investigate the links b

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15

Miettinen, Ville, Jarno Mäkinen, Eero Kolehmainen, Tero Kravtsov, and Lotta Rintala. "Iron Control in Atmospheric Acid Laterite Leaching." Minerals 9, no. 7 (2019): 404. http://dx.doi.org/10.3390/min9070404.

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Iron control in the atmospheric acid leaching (AL) of nickel laterite was evaluated in this study. The aim was to decrease acid consumption and iron dissolution by iron precipitation during nickel leaching. The combined acid leaching and iron precipitation process involves direct acid leaching of the limonite type of laterite followed by a simultaneous iron precipitation and nickel leaching step. Iron precipitation as jarosite is carried out by using nickel containing silicate laterite for neutralization. Acid is generated in the jarosite precipitation reaction, and it dissolves nickel and oth

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16

Alvim-Ferraz, M. C. M., and C. M. Todo-Bom Gaspar. "Impregnated active carbons to control atmospheric emissions." Journal of Colloid and Interface Science 259, no. 1 (2003): 133–38. http://dx.doi.org/10.1016/s0021-9797(02)00171-6.

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17

Alvim-Ferraz, M. C. M., and C. M. Todo-Bom Gaspar. "Impregnated active carbons to control atmospheric emissions." Journal of Colloid and Interface Science 266, no. 1 (2003): 160–67. http://dx.doi.org/10.1016/s0021-9797(03)00648-9.

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18

Planche, M. P., H. Liao, and C. Coddet. "Oxidation control in atmospheric plasma spraying coating." Surface and Coatings Technology 202, no. 1 (2007): 69–76. http://dx.doi.org/10.1016/j.surfcoat.2007.04.053.

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19

Giri, R. K. "Quality control issues in atmospheric motion vectors." Indian Journal of Science and Technology 4, no. 10 (2011): 1126–33. http://dx.doi.org/10.17485/ijst/2011/v4i10.13.

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20

Martin, M. H. "Control and fate of atmospheric trace metals." Environmental Pollution 65, no. 2 (1990): 193. http://dx.doi.org/10.1016/0269-7491(90)90184-e.

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21

Vereshagin, I. P., V. S. Morozov, I. I. Kyrylenko, G. Z. Mirzabekyan, A. V. Orlov, and V. S. Petukhov. "An automatic control system of atmospheric electricity." Journal of Electrostatics 23 (April 1989): 357–60. http://dx.doi.org/10.1016/0304-3886(89)90063-6.

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22

Font, Gabriel I. "Boundary Layer Control with Atmospheric Plasma Discharges." AIAA Journal 44, no. 7 (2006): 1572–78. http://dx.doi.org/10.2514/1.18542.

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23

Chen, Xi, Natalia Andronova, Bram Van Leer, et al. "A Control-Volume Model of the Compressible Euler Equations with a Vertical Lagrangian Coordinate." Monthly Weather Review 141, no. 7 (2013): 2526–44. http://dx.doi.org/10.1175/mwr-d-12-00129.1.

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Abstract Accurate and stable numerical discretization of the equations for the nonhydrostatic atmosphere is required, for example, to resolve interactions between clouds and aerosols in the atmosphere. Here the authors present a modification of the hydrostatic control-volume approach for solving the nonhydrostatic Euler equations with a Lagrangian vertical coordinate. A scheme with low numerical diffusion is achieved by introducing a low Mach number approximate Riemann solver (LMARS) for atmospheric flows. LMARS is a flexible way to ensure stability for finite-volume numerical schemes in both

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24

Cabrerizo, A., J. Dachs, K. C. Jones, and D. Barceló. "Soil-air exchange controls on background atmospheric concentrations of organochlorine pesticides." Atmospheric Chemistry and Physics Discussions 11, no. 9 (2011): 25937–65. http://dx.doi.org/10.5194/acpd-11-25937-2011.

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Abstract. Soils are the major terrestrial reservoir of persistent organic pollutants, and thus net volatilization from soil, when it happens, may exert a control on the atmospheric occurrence and variability of organic pollutants. Here, we report and discuss the concentrations of legacy organochlorine pesticides (OCPs) such as hexachlorobencene (HCB), hexaclorocyclohexanes (HCH) and dichlorodiphenyltrichloroethane (DDT) in the atmosphere and in soils, their measured fugacities in soil, the soil-air partition coefficients (KSA) and soil-air fugacity ratios (fs/fa) in rural background areas of N

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25

Cabrerizo, A., J. Dachs, K. C. Jones, and D. Barceló. "Soil-Air exchange controls on background atmospheric concentrations of organochlorine pesticides." Atmospheric Chemistry and Physics 11, no. 24 (2011): 12799–811. http://dx.doi.org/10.5194/acp-11-12799-2011.

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Abstract. Soils are the major terrestrial reservoir of persistent organic pollutants, and thus net volatilization from soil, when it happens, may exert a control on the atmospheric occurrence and variability of organic pollutants. Here, we report and discuss the concentrations of legacy organochlorine pesticides (OCPs) such as hexachlorobenzene (HCB), hexaclorocyclohexanes (HCH) and dichlorodiphenyltrichloroethane (DDT) in the atmosphere and in soils, their measured fugacities in soil, the soil-air partition coefficients (KSA) and soil-air fugacity ratios (fs/fa) in rural background areas of N

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26

Chung, Samuel W., and Jeong Je Jo. "Pressure Control of HVAC System for Corona Virus." European Journal of Engineering Research and Science 5, no. 4 (2020): 462–68. http://dx.doi.org/10.24018/ejers.2020.5.4.1872.

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Corona Virus is deadly spread out to thousands of healthy people and so strong as to infect to the surrounding people after people. We must keep the deadly virus indoor as much as we can. How? We must not allow the indoor air already contaminated to leak out to the atmosphere, which will transmit to other people. The new virus is so strong and so fast to transmit, it will spread within a few seconds to thousands of people and became patients immediately. To solve the problem, we must build a pressure vessel to keep the virus inside the vessel and not to leak outside. It should be a negative pr

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27

STEFAŃSKI, Konrad, and Marta GRZYB. "Flight of a Guided Aerial Bomb Along a Vertical Plane in Turbulent Atmosphere." Problems of Mechatronics Armament Aviation Safety Engineering 10, no. 3 (2019): 19–30. http://dx.doi.org/10.5604/01.3001.0013.4802.

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The control of a homing flying object, which a guided aerial bomb (GAB) is, takes place in the earth’s atmosphere, which may feature various atmospheric phenomena that are disturbances to the GAB control. The atmospheric disturbances include air turbulences, wind pockets, and wind gusts. For the purpose of the research discussed in this paper, the atmospheric disturbances were qualified as a stochastic process of power spectral density according to the Dryden model. This paper presents a method of controlling a GAB in motion through a turbulent atmosphere of the earth. The GAB was homed to a m

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28

Kunii, Masaru, Kosuke Ito, and Akiyoshi Wada. "Preliminary Test of a Data Assimilation System with a Regional High-Resolution Atmosphere–Ocean Coupled Model Based on an Ensemble Kalman Filter." Monthly Weather Review 145, no. 2 (2017): 565–81. http://dx.doi.org/10.1175/mwr-d-16-0068.1.

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An ensemble Kalman filter (EnKF) that uses a regional mesoscale atmosphere–ocean coupled model was preliminarily examined to provide realistic sea surface temperature (SST) estimates and to represent the uncertainties of SST in ensemble data assimilation strategies. The system was evaluated through data assimilation cycle experiments over a one-month period from July to August 2014, during which time a tropical cyclone (TC) as well as severe rainfall events occurred. The results showed that the data assimilation cycle with the coupled model reproduced SST distributions realistically even witho

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29

Mathes, Armin, Petra Friederichs, and Andreas Hense. "Towards a quality control of precipitation data." Meteorologische Zeitschrift 17, no. 6 (2008): 733–49. http://dx.doi.org/10.1127/0941-2948/2008/0347.

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30

Bony, Sandrine, Bjorn Stevens, David Coppin, et al. "Thermodynamic control of anvil cloud amount." Proceedings of the National Academy of Sciences 113, no. 32 (2016): 8927–32. http://dx.doi.org/10.1073/pnas.1601472113.

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General circulation models show that as the surface temperature increases, the convective anvil clouds shrink. By analyzing radiative–convective equilibrium simulations, we show that this behavior is rooted in basic energetic and thermodynamic properties of the atmosphere: As the climate warms, the clouds rise and remain at nearly the same temperature, but find themselves in a more stable atmosphere; this enhanced stability reduces the convective outflow in the upper troposphere and decreases the anvil cloud fraction. By warming the troposphere and increasing the upper-tropospheric stability,

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31

Liptak, Jessica, and Courtenay Strong. "A Model-Based Decomposition of the Sea Ice–Atmosphere Feedback over the Barents Sea during Winter." Journal of Climate 27, no. 7 (2014): 2533–44. http://dx.doi.org/10.1175/jcli-d-13-00371.1.

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Abstract The feedback between Barents Sea ice and the winter atmosphere was studied in a modeling framework by decomposing it into two sequential boundary forcing experiments. The Community Ice Code (CICE) model was initialized with anomalously high sea ice concentration (SIC) over the Barents Sea and forced with an atmosphere produced by positive SIC anomalies, and CICE was initialized with low Barents Sea SIC and forced with an atmosphere produced by negative SIC anomalies. Corresponding control runs were produced by exposing the same SIC initial conditions to climatological atmospheres, and

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32

Sarwar, Saeed ur Rehman, and Saeed ur Rehman. "Supervising Control for Unmanned Aerial Vehicles." Mathematical Problems in Engineering 2013 (2013): 1–9. http://dx.doi.org/10.1155/2013/564803.

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A small UAV is considered as a test UAV, and its already published aerodynamic data is used for its modeling. Proportional Integral Differential (PID) controller is designed for pitch attitude control. Atmospheric disturbances such as wind shear and turbulence significantly influence the attitude of UAVs. For this study rotary gust is considered as atmospheric disturbance. Pitch response in presence of atmospheric disturbance is presented. In order to improve the performance in presence of atmospheric disturbance, a supervisory mechanism is proposed. Supervisory mechanism is composed of two mo

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33

Kim, Kijung, Bomi Gweon, Minam Lee, Jinseung Choung, Wonho Choe, and Jennifer H. Shin. "PS2-19 Control of fibrosis by atmospheric pressure plasma(PS2: Poster Short Presentation II,Poster Session)." Proceedings of the Asian Pacific Conference on Biomechanics : emerging science and technology in biomechanics 2015.8 (2015): 261. http://dx.doi.org/10.1299/jsmeapbio.2015.8.261.

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34

Yang, Ji-Woong, Jinho Ahn, Edward J. Brook, and Yeongjun Ryu. "Atmospheric methane control mechanisms during the early Holocene." Climate of the Past 13, no. 9 (2017): 1227–42. http://dx.doi.org/10.5194/cp-13-1227-2017.

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Abstract. Understanding processes controlling the atmospheric methane (CH4) mixing ratio is crucial to predict and mitigate future climate changes in this gas. Despite recent detailed studies of the last ∼ 1000 to 2000 years, the mechanisms that control atmospheric CH4 still remain unclear, partly because the late Holocene CH4 budget may be comprised of both natural and anthropogenic emissions. In contrast, the early Holocene was a period when human influence was substantially smaller, allowing us to elucidate more clearly the natural controls under interglacial conditions more clearly. Here w

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35

Baker, Nancy L. "Quality Control for the Navy Operational Atmospheric Database." Weather and Forecasting 7, no. 2 (1992): 250–61. http://dx.doi.org/10.1175/1520-0434(1992)007<0250:qcftno>2.0.co;2.

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36

Fibich, Gadi, Yonatan Sivan, Yosi Ehrlich, et al. "Control of the collapse distance in atmospheric propagation." Optics Express 14, no. 12 (2006): 4946. http://dx.doi.org/10.1364/oe.14.004946.

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37

Rahman, Tawfiqur, Hao Zhou, Liang Yang, and Wanchun Chen. "Pseudospectral Model Predictive Control for Exo-atmospheric Guidance." International Journal of Aeronautical and Space Sciences 16, no. 1 (2015): 64–76. http://dx.doi.org/10.5139/ijass.2015.16.1.64.

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38

Kumar Soni, Rajenda, Santosh Kumar Sar, and Shweta Singh. "APPLICATION OF BIOADSORBENT IN CONTROL OF ATMOSPHERIC POLLUTION." Journal of Applied and Advanced Research 2, no. 1 (2017): 43. http://dx.doi.org/10.21839/jaar.2017.v2i1.54.

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A material that has the ability to extract certain substances from gases, liquids, or solids by causing them to adhere to its surface without changing the physical properties of the adsorbent. Rapid urbanization, population growth, industrial expansion and waste generation from domestic and industrial sources have rendered waste which are hazardous to man and other living resources. Plants absorb carbon dioxide and supply us with oxygen in the process of photosynthesis. At the same time, they reduce pollutants in water and soil. They also remove significant amounts of gaseous pollutants and pa

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39

Bruneau, Ch H., P. Fabrie, and F. Veersé. "Optimal control data assimilation with an atmospheric model." Numerical Functional Analysis and Optimization 18, no. 7-8 (1997): 691–722. http://dx.doi.org/10.1080/01630569708816787.

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40

Marian, S., D. Tsiulyanu, T. Marian, and H. D. Liess. "Chalcogenide-based chemical sensors for atmospheric pollution control." Pure and Applied Chemistry 73, no. 12 (2001): 2001–4. http://dx.doi.org/10.1351/pac200173122001.

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The authors report about characterization of chalcogenide-based thin films, as a materials for gas-sensing applications. The sensing behavior of the AsSTe films was tested with environmental pollutant gases such as NO2, CO, and SO2. A significant sensitivity has been observed for nitrogen dioxide. The detection range for NO2 was between 0.951.9 ppm in ambient air. The response and the recovery time is rapid, with good reproducibility and high sensibility. All the measurements were performed at room temperature. Gas-sensing applications are considered.

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41

Haskins, J. D., F. D. Lopez‐Hilfiker, B. H. Lee, et al. "Anthropogenic Control Over Wintertime Oxidation of Atmospheric Pollutants." Geophysical Research Letters 46, no. 24 (2019): 14826–35. http://dx.doi.org/10.1029/2019gl085498.

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42

Kasparian, J., and J. P. Wolf. "Ultrafast laser spectroscopy and control of atmospheric aerosols." Physical Chemistry Chemical Physics 14, no. 26 (2012): 9291. http://dx.doi.org/10.1039/c2cp23576e.

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43

Lacis, A. A., G. A. Schmidt, D. Rind, and R. A. Ruedy. "Atmospheric CO2: Principal Control Knob Governing Earth's Temperature." Science 330, no. 6002 (2010): 356–59. http://dx.doi.org/10.1126/science.1190653.

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44

Lu, P., and N. X. Vinh. "Minimax optimal control for atmospheric fly-through trajectories." Journal of Optimization Theory and Applications 57, no. 1 (1988): 41–58. http://dx.doi.org/10.1007/bf00939328.

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45

Mai-Prochnow, Anne, Anthony B. Murphy, Keith M. McLean, Michael G. Kong, and Kostya (Ken) Ostrikov. "Atmospheric pressure plasmas: Infection control and bacterial responses." International Journal of Antimicrobial Agents 43, no. 6 (2014): 508–17. http://dx.doi.org/10.1016/j.ijantimicag.2014.01.025.

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46

Verevkin, A. P., and Yu M. Munirov. "Problems in automatic control of atmospheric-vacuum units." Chemistry and Technology of Fuels and Oils 30, no. 11-12 (1994): 392–94. http://dx.doi.org/10.1007/bf00725473.

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47

Duncan Jr., James B., Brian D. Hirth, and John L. Schroeder. "Exploring the complexities associated with full-scale wind plant wake mitigation control experiments." Wind Energy Science 5, no. 2 (2020): 469–88. http://dx.doi.org/10.5194/wes-5-469-2020.

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Abstract. Recent research promotes implementing next-generation wind plant control methods to mitigate turbine-to-turbine wake effects. Numerical simulation and wind tunnel experiments have previously demonstrated the potential benefit of wind plant control for wind plant optimization, but full-scale validation of the wake-mitigating control strategies remains limited. As part of this study, the yaw and blade pitch of a utility-scale wind turbine were strategically modified for a limited time period to examine wind turbine wake response to first-order turbine control changes. Wind turbine wake

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48

Lightfoot, H. Douglas, and Orval A. Mamer. "Back radiation versus CO2 as the cause of climate change." Energy & Environment 28, no. 7 (2017): 661–72. http://dx.doi.org/10.1177/0958305x17722790.

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Robust scientific evidence shows the sun angle controls water vapour content of the atmosphere, the main component of back radiation, as it cycles annually. Water vapour content measured as the ratio of the number of water molecules to CO2 molecules varies from 1:1 near the Poles to 97:1 in the Tropics. The effect of back radiation on Earth’s atmosphere is up to 200 times larger than that of CO2 and works in the opposite direction. Thus, if CO2 has any effect on atmospheric temperature and climate change we show it is negligible. Consequently, current government policies to control atmospheric

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49

Pashinov, E. V. "Space experiment "Convergence": retrieving of atmospheric water vapor profile using of artificial neural networks." Исследования Земли из Космоса, no. 6 (December 21, 2019): 13–25. http://dx.doi.org/10.31857/s0205-96142019613-25.

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The paper is carried out to the investigation of the possibility of retrieving absolute humidity profile of the atmosphere using an artificial neural network based on the modeling of radiometric data of the passive microwave complex MIRS, which is part of the scientific equipment of the space experiment "Convergence". The main approaches to the construction of artificial neural networks are considered. The process of modeling MIRSs radiometric data are described. Selection of optimal characteristics of the neural network is carried out. Necessity of the information about atmospheric temperatur

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Williams, John L., and Reed M. Maxwell. "Propagating Subsurface Uncertainty to the Atmosphere Using Fully Coupled Stochastic Simulations." Journal of Hydrometeorology 12, no. 4 (2011): 690–701. http://dx.doi.org/10.1175/2011jhm1363.1.

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Abstract:

Abstract Feedbacks between the land surface and the atmosphere, manifested as mass and energy fluxes, are strongly correlated with soil moisture, making soil moisture an important factor in land–atmosphere interactions. It is shown that a reduction of the uncertainty in subsurface properties such as hydraulic conductivity (K) propagates into the atmosphere, resulting in a reduction in uncertainty in land–atmosphere feedbacks that yields more accurate atmospheric predictions. Using the fully coupled groundwater-to-atmosphere model ParFlow-WRF, which couples the hydrologic model ParFlow with the

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