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1

HILEMAN, BETTE. "GREENHOUSE GASES." Chemical & Engineering News 81, no. 4 (January 27, 2003): 12. http://dx.doi.org/10.1021/cen-v081n004.p012.

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2

Shilling, Fraser. "Greenhouse gases." Nature 375, no. 6533 (June 1995): 626. http://dx.doi.org/10.1038/375626b0.

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3

Chilingar, G. V., O. G. Sorokhtin, L. Khilyuk, and M. V. Gorfunkel. "Greenhouse gases and greenhouse effect." Environmental Geology 58, no. 6 (November 14, 2008): 1207–13. http://dx.doi.org/10.1007/s00254-008-1615-3.

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4

Hatfield, Craig Bond. "Reducing Greenhouse Gases." Science 271, no. 5248 (January 26, 1996): 431. http://dx.doi.org/10.1126/science.271.5248.431-a.

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5

Pollock, Chris. "Agricultural greenhouse gases." Nature Geoscience 4, no. 5 (April 29, 2011): 277–78. http://dx.doi.org/10.1038/ngeo1145.

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6

Hatfield, C. B. "Reducing Greenhouse Gases." Science 271, no. 5248 (January 26, 1996): 431a. http://dx.doi.org/10.1126/science.271.5248.431a.

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7

HILEMAN, BETTE. "REDUCING GREENHOUSE GASES." Chemical & Engineering News 77, no. 39 (September 27, 1999): 25. http://dx.doi.org/10.1021/cen-v077n039.p025.

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8

HILEMAN, BETTE. "REDUCING GREENHOUSE GASES." Chemical & Engineering News 78, no. 43 (October 23, 2000): 11. http://dx.doi.org/10.1021/cen-v078n043.p011.

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9

REISCH, MARC S. "MONITORING GREENHOUSE GASES." Chemical & Engineering News 88, no. 32 (August 9, 2010): 10–13. http://dx.doi.org/10.1021/cen080310153359.

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10

Herzog, Howard, Baldur Eliasson, and Olav Kaarstad. "Capturing Greenhouse Gases." Scientific American 282, no. 2 (February 2000): 72–79. http://dx.doi.org/10.1038/scientificamerican0200-72.

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11

Lashof, Daniel A. "Reducing greenhouse gases." Nature 374, no. 6520 (March 1995): 300. http://dx.doi.org/10.1038/374300a0.

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12

Subak, S. E. "Reducing greenhouse gases." Nature 374, no. 6520 (March 1995): 300. http://dx.doi.org/10.1038/374300b0.

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13

Scarratt, J. B. "Greenhouse Managers: Beware Combustion Fumes in Container Greenhouses." Forestry Chronicle 61, no. 4 (August 1, 1985): 308–11. http://dx.doi.org/10.5558/tfc61308-4.

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The combustion of fossil fuels produces a number of gases that can be phytotoxic to plants. Managers of container nurseries should be alert to the fact that entry of these combustion gases into the greenhouse environment can have serious effects upon tree seedlings. At high concentrations, seedlings may be severely damaged or killed outright. Chronic exposure to low levels of pollution can significantly reduce seedling growth even when no other visible symptoms are present. Careful design and layout of greenhouse facilities, and vigilance in the operation of heating equipment, generators and vehicles, are essential to avoid the risk of pollution damage. The effects of an incident in which jack pine (Pinus banksiana Lamb.) container stock was exposed to non-lethal concentrations of combustion gasses are described.
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14

Cole, Jonathan J. "Microorganisms and Greenhouse Gases." Ecology 74, no. 2 (March 1993): 637–38. http://dx.doi.org/10.2307/1939331.

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15

Burke, Maria. "Trading in greenhouse gases." Environmental Science & Technology 37, no. 7 (April 2003): 124A—125A. http://dx.doi.org/10.1021/es0324104.

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16

HILEMAN, BETTE. "GREENHOUSE GASES WARMING OCEANS." Chemical & Engineering News 79, no. 16 (April 16, 2001): 7. http://dx.doi.org/10.1021/cen-v079n016.p007a.

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17

HILEMAN, BETTE. "ACCOUNTING FOR GREENHOUSE GASES." Chemical & Engineering News 79, no. 46 (November 12, 2001): 21. http://dx.doi.org/10.1021/cen-v079n046.p021.

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18

PRASETYADEWI, Venita, Achmad NURMANDI, Helen Dian FRIDAYANI, and Muhammad Eko ATMOJO. "Bibliometric Analysis of Renewable Energy Use in Low Carbon Development." International Journal of Environmental, Sustainability, and Social Science 5, no. 3 (May 31, 2024): 577–91. http://dx.doi.org/10.38142/ijesss.v5i3.938.

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Greenhouse gases are gases trapped in the earth's atmosphere that cause the earth's surface temperature to become hot, when during the day the sun emits rays that can penetrate into the earth's atmosphere and warm the earth while at night the earth's surface becomes cold and can release the earth's heat back into the air, with the presence of these gases so that they can reflect the earth's heat back to the earth again because that is called greenhouse gases. Greenhouse gases that occur due to excessive human activity resulting in the release of a number of greenhouse gases into the earth's atmosphere. Greenhouse gases are caused by excessive human activity that results in the release of a number of greenhouse gases into the earth's atmosphere. Greenhouse gases increased in 2020 due to factors such as the burning of coal, oil and natural gas produced from Indonesia's industrial energy sector. Then there was a decrease in gas emissions, due to Covid-19 in the use of fuel in the transportation sector, but in 2021 until now there has been an increase caused by the energy sector and industrial activities. Based on this, this analysis focuses on government efforts to reduce greenhouse gases. In this analysis, using bibliometric analysis as a method used to analyse how trends and developments regarding research on greenhouse gases. The results of this analysis refer the government's real steps by using renewable energy such as solar energy and geothermal energy to reduce the effects of greenhouse gases.
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19

Jeffry, Luqman, Mei Yin Ong, Saifuddin Nomanbhay, M. Mofijur, Muhammad Mubashir, and Pau Loke Show. "Greenhouse gases utilization: A review." Fuel 301 (October 2021): 121017. http://dx.doi.org/10.1016/j.fuel.2021.121017.

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20

Bonn, Dorothy. "Greenhouse Gases Warmed Prehistoric Oceans." Frontiers in Ecology and the Environment 2, no. 1 (February 2004): 5. http://dx.doi.org/10.2307/3868277.

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21

Boesch, Hartmut, Yi Liu, Johanna Tamminen, Dongxu Yang, Paul I. Palmer, Hannakaisa Lindqvist, Zhaonan Cai, et al. "Monitoring Greenhouse Gases from Space." Remote Sensing 13, no. 14 (July 8, 2021): 2700. http://dx.doi.org/10.3390/rs13142700.

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The increase in atmospheric greenhouse gas concentrations of CO2 and CH4, due to human activities, is the main driver of the observed increase in surface temperature by more than 1 °C since the pre-industrial era. At the 2015 United Nations Climate Change Conference held in Paris, most nations agreed to reduce greenhouse gas emissions to limit the increase in global surface temperature to 1.5 °C. Satellite remote sensing of CO2 and CH4 is now well established thanks to missions such as NASA’s OCO-2 and the Japanese GOSAT missions, which have allowed us to build a long-term record of atmospheric GHG concentrations from space. They also give us a first glimpse into CO2 and CH4 enhancements related to anthropogenic emission, which helps to pave the way towards the future missions aimed at a Monitoring & Verification Support (MVS) capacity for the global stock take of the Paris agreement. China plays an important role for the global carbon budget as the largest source of anthropogenic carbon emissions but also as a region of increased carbon sequestration as a result of several reforestation projects. Over the last 10 years, a series of projects on mitigation of carbon emission has been started in China, including the development of the first Chinese greenhouse gas monitoring satellite mission, TanSat, which was successfully launched on 22 December 2016. Here, we summarise the results of a collaborative project between European and Chinese teams under the framework of the Dragon-4 programme of ESA and the Ministry of Science and Technology (MOST) to characterize and evaluate the datasets from the TanSat mission by retrieval intercomparisons and ground-based validation and to apply model comparisons and surface flux inversion methods to TanSat and other CO2 missions, with a focus on China.
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22

Zavadoff, Breanna L. "Greenhouse gases strengthen atmospheric rivers." Nature Climate Change 11, no. 11 (October 4, 2021): 904–5. http://dx.doi.org/10.1038/s41558-021-01181-9.

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23

Rohrman, Douglass F. "Regulating greenhouse gases, part II." Frontiers in Ecology and the Environment 7, no. 5 (June 2009): 279. http://dx.doi.org/10.1890/1540-9295-7.5.279.

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24

Herman, Benjamin M., Xubin Zeng, Tom Chase, and Roger Pielke. "More Heat Over Greenhouse Gases." Physics Today 55, no. 5 (May 2002): 14. http://dx.doi.org/10.1063/1.1485563.

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25

Ledley, Tamara S., Eric T. Sundquist, Stephen E. Schwartz, Dorothy K. Hall, Jack D. Fellows, and Timothy L. Killeen. "Climate change and greenhouse gases." Eos, Transactions American Geophysical Union 80, no. 39 (September 28, 1999): 453–58. http://dx.doi.org/10.1029/99eo00325.

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26

Kaiser, J. "ENVIRONMENT:Pollution Permits for Greenhouse Gases?" Science 282, no. 5391 (November 6, 1998): 1025. http://dx.doi.org/10.1126/science.282.5391.1025.

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27

Whitten, Robert C. "Greenhouse Gases Warm Things Up." Physics Today 54, no. 12 (December 2001): 12. http://dx.doi.org/10.1063/1.1445525.

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28

Goth, Gregory. "Chipping away at greenhouse gases." Communications of the ACM 54, no. 2 (February 2011): 13–15. http://dx.doi.org/10.1145/1897816.1897823.

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29

Mitchell, J. F. B. "Local effects of greenhouse gases." Nature 332, no. 6163 (March 1988): 399–400. http://dx.doi.org/10.1038/332399a0.

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30

Anderson, Alun. "US legislators attack greenhouse gases." Nature 335, no. 6191 (October 1988): 583. http://dx.doi.org/10.1038/335583b0.

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31

Smith, H. Jesse. "Greenhouse gases drove African rainfall." Science 346, no. 6214 (December 4, 2014): 1195.15–1195. http://dx.doi.org/10.1126/science.346.6214.1195-o.

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32

Levi, Barbara Goss. "Greenhouse Gases Warm Things Up." Physics Today 54, no. 12 (December 2001): 12–13. http://dx.doi.org/10.1063/1.4796237.

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33

Robson, Robert E. "More Heat Over Greenhouse Gases." Physics Today 55, no. 5 (May 2002): 14–15. http://dx.doi.org/10.1063/1.4796724.

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34

HILEMAN, BETTE. "U.S. ACTIONS ON GREENHOUSE GASES." Chemical & Engineering News 85, no. 45 (November 5, 2007): 20–24. http://dx.doi.org/10.1021/cen-v085n045.p020.

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35

ZURER, PAMELA. "Greenhouse gases impeding ozone recovery." Chemical & Engineering News 76, no. 15 (April 13, 1998): 12. http://dx.doi.org/10.1021/cen-v076n015.p012.

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36

HILEMAN, BETTE. "HOW TO REDUCE GREENHOUSE GASES." Chemical & Engineering News 80, no. 21 (May 27, 2002): 37–41. http://dx.doi.org/10.1021/cen-v080n021.p037.

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37

HESS, GLENN. "STATES THWARTED ON GREENHOUSE GASES." Chemical & Engineering News Archive 83, no. 30 (July 25, 2005): 10. http://dx.doi.org/10.1021/cen-v083n030.p010a.

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38

Covey, K. R., C. P. Bueno de Mesquita, B. Oberle, D. S. Maynard, C. Bettigole, T. W. Crowther, M. C. Duguid, et al. "Greenhouse trace gases in deadwood." Biogeochemistry 130, no. 3 (October 7, 2016): 215–26. http://dx.doi.org/10.1007/s10533-016-0253-1.

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39

Moomaw, William R. "Industrial emissions of greenhouse gases." Energy Policy 24, no. 10-11 (October 1996): 951–68. http://dx.doi.org/10.1016/s0301-4215(96)80360-0.

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40

Zhong, Wenyi, J. D. Haigh, and J. A. Pyle. "Greenhouse gases in the stratosphere." Journal of Geophysical Research: Atmospheres 98, no. D2 (February 20, 1993): 2995–3004. http://dx.doi.org/10.1029/92jd02024.

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41

ABELSON, P. H. "Greenhouse Role of Trace Gases." Science 231, no. 4743 (March 14, 1986): 1233. http://dx.doi.org/10.1126/science.231.4743.1233.

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42

Belic, Dragoljub. "Global warming and greenhouse gases." Facta universitatis - series: Physics, Chemistry and Technology 4, no. 1 (2006): 45–55. http://dx.doi.org/10.2298/fupct0601045b.

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Global warming or Climate change refers to long-term fluctuations in temperature, precipitation, wind, and other elements of the Earth's climate system. Natural processes such as solar-irradiance variations, variations in the Earth's orbital parameters, and volcanic activity can produce variations in climate. The climate system can also be influenced by changes in the concentration of various gases in the atmosphere, which affect the Earth's absorption of radiation.
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43

Birat, J. P., J. M. Delbecq, E. Hess, and D. Huin. "Slag, steel and greenhouse gases." Revue de Métallurgie 99, no. 1 (January 2002): 13–21. http://dx.doi.org/10.1051/metal:2002177.

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44

Mequignon, Marc, Hassan Ait Haddou, Françoise Thellier, and Marion Bonhomme. "Greenhouse gases and building lifetimes." Building and Environment 68 (October 2013): 77–86. http://dx.doi.org/10.1016/j.buildenv.2013.05.017.

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45

Daniil, Terpugov, and Terpugov Grigory. "ChemInform Abstract: Greenhouse Gases Trapping." ChemInform 45, no. 21 (May 8, 2014): no. http://dx.doi.org/10.1002/chin.201421294.

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46

Grabarczyk, Robert, and Sławomir Grabarczyk. "Cumulative Energy Demand and Carbon Footprint of the Greenhouse Cultivation System." Applied Sciences 12, no. 17 (September 1, 2022): 8786. http://dx.doi.org/10.3390/app12178786.

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The paper describes the influence of horticultural production in greenhouses under Polish climate conditions on energy consumption, contributing to greenhouse gas emissions and global warming. Four scenarios were studied, two of which were non-renewable fuels: coal and natural gas, while the other two were renewable energy sources: wood pellets and wood chips, to identify opportunities for reducing energy costs and greenhouse gas emissions. Cumulative energy demand was defined to assess these four scenarios. The environmental impact was determined using the carbon footprint of the principal greenhouse gases emitted and using CO2 as the reference gas (CO2-equivalents). Renewable energy sources in greenhouse production can reduce the cumulative energy demand by 83.3% and greenhouse gas emissions by 95% compared to the coal-burning scenario. The presented research results relate to a greenhouse intended for growing flowers in pots, which has not been conducted so far. The article also updates the data on the environmental impact of crops grown in greenhouses located in Poland. The study provides important information for horticultural producers, mainly due to increasing competition and consumer awareness of the origin of products. Renewable energy sources in horticulture reveal a great potential in the reduction in greenhouse gases, and thus may become an inspiration to look for new solutions in this area.
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47

Markanda, Sangeet, and R. K. Aggarwal R K Aggarwal. "Low cost power generation using greenhouse gases in thermocouple." Indian Journal of Applied Research 3, no. 7 (October 1, 2011): 570–72. http://dx.doi.org/10.15373/2249555x/july2013/179.

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48

Smith, Irene. "Carbon Dioxide and Climatic Change." Energy Exploration & Exploitation 6, no. 6 (December 1988): 465–75. http://dx.doi.org/10.1177/014459878800600606.

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Certainties and uncertainties in the issue of the greenhouse gases are discussed. It is an established fact that the concentrations of these trace gases — CO2 chlorofluorocarbons (CFC), methane, nitrous oxide and ozone — are increasing in the lower atmosphere as a result of human activities. The contribution of coal use to the greenhouse effect is about 15 to 20%. Future emissions of the greenhouse gases form one of the greatest sources of uncertainty. The potential for reducing emissions of the greenhouse gases is discussed. While steps are being taken to control CFC, the greenhouse gases with the greatest rate of increase, the scope for reducing CO2 emissions is limited. Climatic model results suggest that there will be a noticeable global warming in one or two decades with more uncertain regional changes. Observations are consistent with these results but there is as yet no conclusive causal link with increases in the greenhouse gases.
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49

Jomarie C. Salar and Emil Martin N. Pelias. "The Complexity of Global Tourism and Greenhouse Gases." Journal of Educational and Human Resource Development (JEHRD) 8 (December 30, 2020): 149–65. http://dx.doi.org/10.61569/y54zhf10.

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This study investigates the complexity of global tourism (tourism arrivals and tourism departures) of 93 countries by considering the greenhouse gases characteristics (carbon dioxide emission, nitrous oxide, methane, and fluorinated gas) in 2012 using a complex adaptive system approach. The results of the study indicated that greenhouse gases characteristics and global tourism interact in a nonlinear manner. Results showed that the indices of global tourism are unpredictable for a certain period, and in the long run, will drop down to zero once the greenhouse gases characteristics reach its maximum for the low-income and lower middle-income countries. However, in highly developed countries, the level of greenhouse gases characteristics does not matter to global tourism. Global tourism is not dependent on how high or low the greenhouse gases characteristics of highly developed countries are, which implies that other factors have influenced the global tourism of these countries even if the greenhouse gases characteristics are high. It is suggested that the governments in low income and lower-middle-income countries which significantly rely on tourism should be responsive by inventing and adopting green technology, promoting eco-friendly operation and adopting sustainable tourism to protect the environment and promote renewable energy which will help lessen the greenhouse gases emitted by various production industries.
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50

Zhu, Xiao-cong, Dong-rui Di, Ming-guo Ma, and Wei-yu Shi. "Stable Isotopes in Greenhouse Gases from Soil: A Review of Theory and Application." Atmosphere 10, no. 7 (July 6, 2019): 377. http://dx.doi.org/10.3390/atmos10070377.

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Greenhouse gases emitted from soil play a crucial role in the atmospheric environment and global climate change. The theory and technique of detecting stable isotopes in the atmosphere has been widely used to an investigate greenhouse gases from soil. In this paper, we review the current literature on greenhouse gases emitted from soil, including carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O). We attempt to synthesize recent advances in the theory and application of stable isotopes in greenhouse gases from soil and discuss future research needs and directions.
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