The Climate and Global Warming Responses to the Changing Greenhouse Gas Concentration in the Atmosphere
##plugins.themes.academic_pro.article.main##
Abstract
Increase of the World temperature throughout the Earth is called Global warming. Studies have shown that Temperature of the earth have risen, if do not stopped on time, it will rise further. The reason of this global warming are Greenhouse gases like, Nitrous Oxide, Carbon Dioxide, Methane, Sulphurehexafloride, Nitrogen Trifloride, Hydrofluorocarbon, Perfluorocarbon. Global warming of the Nitrous oxide is 265 and can stay up to 121 years in the atmosphere. It has 298 times more potential in the warming up of the glob than Carbon dioxide, which are being produced by human’s industrial activities. Therefore Carbon dioxide is being produced with the burning of the fossil fuels and the ability of the Carbon dioxide in global warming 1. Methane is a gas which is being produced by the burning of the organic materials. Sulphur Hexafluoride is also a strong gas of the greenhouse gases and is unburnable and is able to wipe out the infrared waves. It keeps the earth warm for a long time. Nitrogentrichloride is a gas which causes skin and eye’s disease. Therefore, every molecule of the Hydrofluorocarbon is much stronger as compare to the Carbon dioxide. It prevents the distraction of the Ozone layer. On the other side, perfluorocarbon is a gas which has the ability to wipe out the Ozone Layer. Greenhouse is a place which protects Plants from direct sunlight. Greenhouse gases cause many problems which can cause climate change, like melting of the glacier, rise in the sea water and Increase in storms. In the reduction of the greenhouse gases, a number of processes have been started like using renewable energy, using Bicycle, Using local transportations, protecting forests and using air filters.
Keywords
Increase, Global, Warming, Climate, Change, Concentration, Green, House##plugins.themes.academic_pro.article.details##
References
- Duarte-Galvan, C., Torres-Pacheco, I., Guevara-Gonzalez, R. G., Romero-Troncoso, R. J., Contreras-Medina, L. M., Rios-Alcaraz, M. A., & Millan-Almaraz, J. R. (2012). Advantages and disadvantages of control theories applied in greenhouse climate control systems. Spanish Journal of Agricultural Research, 10(4), 926-938.
- Jeffry, L., Ong, M. Y., Nomanbhay, S., Mofijur, M., Mubashir, M., & Show, P. L. (2021). Greenhouse gases utilization: A review. Fuel, 301, 121017.)
- Lammel, G., & Graßl, H. (1995). Greenhouse effect of NO X. Environmental Science and Pollution Research, 2, 40-45.
- Mahanti, P., Kumar, S., & Patra, J. K. (2017). Biosurfactants: An agent to keep environment clean. Microbial Biotechnology: Volume 1. Applications in Agriculture and Environment, 413-428.
- Mitchell, J. F. (1989). The “greenhouse” effect and climate change. Reviews of Geophysics, 27(1), 115-139.
- Nazaroff, W. W. (2013). Exploring the consequences of climate change for indoor air quality. Environmental Research Letters, 8(1), 015022.
- Olivier, J. G., Schure, K. M., & Peters, J. A. H. W. (2017). Trends in global CO2 and total greenhouse gas emissions. PBL Netherlands Environmental Assessment Agency, 5, 1-11.
- Shah, S. (2020). Analysis of Greenhouse Gases. arXiv preprint arXiv:2003.11916.
- Tohka, A. (2005). The GAINS model for greenhouse gases-version 1.0: HFC, PFC and SF6.
- Trenberth, K. E., & Fasullo, J. T. (2013). An apparent hiatus in global warming?. Earth's Future, 1(1), 19-32.
- Tsai, W. T. (2008). Environmental and health risk analysis of nitrogen trifluoride (NF3), a toxic and potent greenhouse gas. Journal of Hazardous Materials, 159(2-3), 257-263.
- Ulyatt, M. J., Clark, H., & Lassey, D. K. R. (2002, January). Methane and climate change. In Proceedings of the New Zealand Grassland Association (pp. 153-157).