earth’s climate
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2022 ◽  
Author(s):  
Phạm Hà Trang

Climate change is a global challenge, directly affecting ecosystems, environmental resources, and human life. One of its consequences is the problem of sea and ocean surface area, sea level is increasing day by day. In the long term, global mean sea level will continue to change continuously. The birth of the industrial revolution has made the Earth warmer and warmer, followed by many different causes leading to the rapid increase of global sea level: melting ice, expansion of the sea. water and changes in the Earth's climate system, costing the global economy trillions of dollars with many development consequences.


2022 ◽  
Vol 2152 (1) ◽  
pp. 012001
Author(s):  
Heng Li

Abstract Increase of atmospheric aerosols has a profound impact on the Earth’s climate. It’s also one of the crucial factors that cuasesd more fequent air pollution events in China. Monthly average Aerosol Optical Depth (AOD) from MODIS and UltraViolet Absorbing aerosol Index (UVAI) from OMI during 2011 to 2019 are used to analyse the trend of absorption and total aerosol optical properties over three typical provinces of China, namely Shandong, Gansu and Guangdong provinces. The results show the average annual AOD of the three provinces are all decreasing while UVAI rises during this period. In addition, the monthly variation of AOD and UVAI are also obviously different over these provinces. In particular, the peak value of AOD appeared in July and the trough appeared in December over Shandong Province. And the peak appeared in April over Gansu Province, but AOD decrease slower then over Shandong Province. And there were two peaks in April and August over Guangdong Province. For UVAI, the peaks over Shandong and Gansu provinces both occur in January, while that over Guangdong Province appears in March. Above mentioned differences in the long-term trend and monthly variation of AOD and UVAI might be closely related to the meteorological conditions and aerosol emission of these three provinces.


2021 ◽  
pp. 528-534
Author(s):  
Petro Nevodovskyi ◽  
Oleksandr Ovsak ◽  
Anatoliy Vidmachenko ◽  
Оrest Ivakhiv ◽  
Oleksandr Zbrutskyi ◽  
...  

Earth’s climate changes are the result of natural changes in the energy balance of Sun irradiation and influence of anthropogenic factors on the variations of ozone layer thickness and stratospheric aerosol abundance. It is developed a miniature polarimeter for satellite polarimetric experiments in the ultraviolet region of the sunlight spectrum. The main task of this device is to the obtain an information on the stratospheric aerosol physical properties. We tested this polarimeter on a bench specially designed and manufactured as well. It is possible to measure by it the phase dependences of the degree of linear polarization (DLP) of solar radiation scattered by the Earth’s atmosphere. A set of special computer programs was developed for comparing the spectral polarimetric measurements DLP data of cloudless sky with model calculations of DLP for the artificial gas-aerosol medium. Thus, the prototype of satellite polarimeter as well as special computer programs make it possible to study the Earth’s atmosphere aerosol physical characteristics.


2021 ◽  
Author(s):  
Guillermo Nicolás Murray Tortarolo

Earth’s surface temperature oscillated greatly throughout time. From near congelation during “snowball Earth” 2.9Gya to an ice-free world in the Paleocene-Eocene Thermal maximum 55Mya. These changes have been forced by internal (e.g. changes in the chemical composition of the atmosphere) or external (e.g. changes in solar luminosity) drivers that varied through time. Thus, if we understand how the radiation budget evolved in different times, we can closely calculate past global climate; a fundamental comparison to situate current climate change in the context Earth’s history. Here I present an analytical framework employing a simple energy balance derived from the Stephan-Boltzmann law, that allows for quick comparison between drivers of global temperature and at multiple moments in the history of our planet. My results show that current rates of increase in global temperature are at least four times faster than any previous warming event.


2021 ◽  
Author(s):  
Anthony Dosseto ◽  
Nathalie Vigier ◽  
Renaud Joannes-Boyau ◽  
Ian Moffat ◽  
Tejpal Singh ◽  
...  

Chemical weathering of continental rocks plays a central role in regulating the carbon cycle and the Earth’s climate (Walker et al., 1981; Berner et al., 1983), accounting for nearly half the consumption of atmospheric carbon dioxide globally (Beaulieu et al., 2012). However, the role of climate variability on chemical weathering is still strongly debated. Here we focus on the Himalayan range and use the lithium isotopic composition of clays in fluvial terraces to show a tight coupling between climate change and chemical weathering over the past 40 ka. Between 25 and 10 ka ago, weathering rates decrease despite temperature increase and monsoon intensification. This suggests that at this timescale, temperature plays a secondary role compared to runoff and physical erosion, which inhibit chemical weathering by accel-erating sediment transport and act as fundamental controls in determining the feedback between chemical weathering and atmospheric carbon dioxide.


Entropy ◽  
2021 ◽  
Vol 23 (12) ◽  
pp. 1648
Author(s):  
Amelia Carolina Sparavigna

Image analysis basically refers to any extraction of information from images, which can be as simple as QR codes required in logistics and digital certifications or related to large and complex datasets, such as the collections of images used for biometric identification or the sets of satellite surveys employed in the monitoring of Earth’s climate changes [...]


2021 ◽  
Author(s):  
Julia Schubert

Notions of the impending climate crisis have pushed a set of highly contested techno-scientific measures onto policy agendas around the world. Suggestions to deliberately alter, to engineer, the Earth’s climate have gained political currency in recent years not as a positive vision of techno-scientific innovation, but as a daunting measure of last resort. The controversial status of various so-called climate engineering proposals raises a simple, yet pressing question: How has it has come to this? And, more specifically, how did such contested measures earn their place on policy agendas, despite enormous scientific complexities and fierce political contestation? Global societal problems, such as climate change, financial crises, or pandemics have brought the political relevance of scientific expertise to the foreground. This book speaks to scholarship in sociology and science studies, seeking to illuminate the essential entanglements between efforts to understand and efforts to govern such problems. By giving climate engineering a life of its own and following its dynamic trajectory as a contested object of expert work, this book sheds light on the reflexive and historically contingent interplay of science and politics as two distinct, yet increasingly interdependent, realms of society.


2021 ◽  
Author(s):  
Jorge Sánchez-Sesma

Abstract. This work provides a hypothesis of the links between the multi-millennia scale recurrent solar and tidal influences and Earth's climate lagged responses, associated with the oceanic transport mechanisms with a variable modulation. As a part of this hypothesis, empirical and simple, non-linear lagged models are proposed for five of the most representative Earth's climate variables (a continental tropical temperature, an Antarctic temperature [at James Ross Island], the Greenland temperature, the global temperature and the southeast asian monsoon) with multi-millennia records to account for the lagged responses to solar forcing. The proposed models implicitely include a well-known oceanic heat transport mechanism: the Ocean Conveyor Belt. This oceanic mechanism appears to generate a climate modulation through the intensity of the ocean/atmosphere circulation, and a heat and mass transport, with a consequent climate lag of several thousands of years. Tidal forcing is also considered for global temperature modelling and forecast. The consequent millennia-scale global forecasts, after being integrated/verified with an accumulated ocean travelled distance from the tropical East Pacific, and with a double evaluation of the tidal influences based on similarities and on the NASA’s solar system astronomical dynamics, indicates a cooling for the next century, and gentle oscillations over the next millennia. Our preliminary results that strongly suggest that millennial scale changes in solar activity induce circulation and thermal global impacts, also suggest that the Younger Dryas event, may be influenced by the lagged outcomes of solar driven changes in the tropical Pacific, and by tidal influences. The detected Earth's climate delayed responses, that have been working in the past and present climates, and will be working in the future climates, must be, as soon as possible, independently verified and theoretically sustained, before to be fully included in a multi-scale climate models as a scientific theory. A final example for the global temperature record over the last 170 years demonstrates with experimental results for the twenty first century evolution the convenience of a multi-scale climate modelling with contrasting lower values compared with the IPCC global temperature scenarios.


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