The physical process of parturition.

Author(s):  
M. C. G. Davies Morel
Keyword(s):  
Author(s):  
Christian Sternad

AbstractAging is an integral part of human existence. The problem of aging addresses the most fundamental coordinates of our lives but also the ones of the phenomenological method: time, embodiment, subjectivity and intersubjectivity, and even the social norms that grow into the very notion of aging as such. In my article, I delineate a phenomenological analysis of aging and show how such an analysis connects with the debate concerning personal identity: I claim that aging is not merely a physical process, but is far more significantly also a spiritual one as the process of aging consists in our awareness of and conscious relation to our aging. This spiritual process takes place on an individual and on a social level, whereas the latter is the more primordial layer of this experience. This complicates the question of personal identity since it will raise the question in two ways, namely who I am for myself and who I am for the others, and in a further step how the latter experience shapes the former. However, we can state that aging is neither only physical nor only spiritual. It concerns my bodily processes as it concerns the complex reflexive structure that relates my former self with my present and even future self.


IEEE Access ◽  
2020 ◽  
Vol 8 ◽  
pp. 3115-3122
Author(s):  
Danlei Ye ◽  
Xin Jiang ◽  
Guanying Huo ◽  
Cheng Su ◽  
Zehong Lu ◽  
...  

2018 ◽  
Author(s):  
Jinhui Gao ◽  
Bin Zhu ◽  
Hui Xiao ◽  
Hanqing Kang ◽  
Chen Pan

Abstract. As an important solar-radiation absorbing aerosol, the effect of black carbon (BC) on surface ozone, by influencing photolysis rate, has been widely discussed by offline model studies. However, BC-boundary layer (BL) interactions also influence surface ozone. Using the online model simulations and processes analysis, we demonstrate the significant impact of BC-BL interaction on surface ozone. The absorbing effect of BC heats the air above the BL and suppresses BL development, which eventually leads to changes in the contributions of ozone through chemical and physical processes (photochemistry, vertical mixing, and advection). Different from previous offline model studies, BL suppression leads large amounts of ozone precursors being confined below the BL which offsetting the influence from the reduction of photolysis rate, thus enhancing ozone photochemical formation before noon. Furthermore, the changes in physical process show a more significant influence on surface ozone. The weakened turbulence entrains much less ozone from the overlying ozone-rich air down to surface. As a result, the net contribution of ozone from physical and chemical processes leads to surface ozone reduction before noon. The maximum reduction reaches to 16.4 ppb at 12:00. In the afternoon, the changes in chemical process are small which influence inconspicuously to surface ozone. However, physical process still influences the surface ozone significantly. Due to the delayed development of the BL, less vertically mixed BL continues to show an obvious ozone gradient near the top of the BL. Therefore, more ozone aloft can be entrained down to the surface, offsetting the surface ozone reduction. Comparing all the changes in the contributions of processes, the change in the contribution of vertical mixing plays a more important role in impacting surface ozone. Our results show the great impacts of BC-BL interactions on surface ozone. And more attention should be paid on the mechanism of aerosol-BL interactions when we deal with the ozone pollution control in China.


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