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The Centre for Business Taxation has a number of sources of funding from both public and private sectors. The views expressed here are those of the authors; the Centre has no corporate views. Grubert, ; Overesch and Schreiber, forthcoming. Huizinga and Laeven for a similar approach. The rest of the paper is structured as follows: Section 2 presents the data set used for the analysis and Section 3 describes the estimation strategy.
This finding is consistent with the fact that the stratospheric intrusions bringing O3 into the troposphere reach their seasonal maximum in the summer 27 , This is primarily due to unusually strong winds associated with the polar and subtropical jet streams over the east Asian coast and the persistence of cyclogenesis over the western Pacific, resulting in frequent tropopause folding and thus significant intrusion of O3 into the troposphere 10 , 25 , 29 , 30 , 31 , The air remaining in the fold of the upper troposphere moves towards the jet exit regions and re-enters the lower stratosphere.
However, stretching stratospheric intrusions to smaller scales, some of which go deeper into the troposphere, leads to irreversible transport 1 , 10 , 33 , 34 , 35 , 36 , Such deep intrusions of stratospheric air down to the lower troposphere or even to the surface are relevant to tropospheric chemistry 8 , 9 , Ozone, however, is reactive and with numerous sources at the ground level, which makes the use of ozone for the irreversible branch rather ambiguous.
The anomaly in CO2 is potentially also a powerful tracer for improving our understanding of the carbon cycle One advantage of using CO2 is that this species is inert in the free troposphere; the isotopic composition of CO2 can be modified at the surface and in the middle and upper atmospheres only.
It has been discovered that some atmospheric species follow a very different relation. As O3 and CO2 are strongly coupled in the stratosphere and isotopically anomalous CO2 can be produced in the middle atmosphere only, one may obtain a better constraint for stratospheric O3 at the surface by measuring the isotopic composition of CO2.
The exchange was carried out in a reaction tube made of quartz, 60 cm in length and 6. The heating zone is about 15 cm. Columns 3 and 4 depict the regression results for the low-tax subsidiary sample. In a second robustness check, we moreover assess whether our results are driven by heterogeneity of multinational groups in other dimensions. Thus, in recent year an increasing number of countries have introduced or tightened anti-shifting legislations, for example strengthened thin-capitalization rules or introduced transfer price documentation requirements see e.
Buettner, et al.
Budd, J. Konings and M.
Buettner, T. Wamser, M.
Overesch, and U. It is also important to understand how CO2 concentrations in the atmosphere of urban source regions change with time. Attempts with applying remote sensing technique to probe CO2 at local scales have been shown to be promising e. Major sources of CO2 are anthropogenic emissions from fossil fuel combustion, biomass burning, and plant and soil respiration; and major sinks are due to terrestrial and oceanic uptakes.
So far, no isotopic study in atmospheric CO2 has been conducted systematically in any part of Taiwan. On per capita basis, Taiwan A major part of this emission is contributed by big cities such as Taipei.
Being in the down winds of China and southeast Asia countries, Taiwan is an ideal place for assessing regional anthropogenic impacts. A systematic source speciation is also important for the current deep decarbonization initiative of Taiwan. The emphases of the available studies in the region are mainly focused on the influences of pollutants from the Asian land masses on the region e. The region near the sea level encounters prevailing wind from northeast in winter—spring November—May and from southwest during summer June—September Chang et al.
It is well known that northwestern Pacific region is affected by the pollutants from Asian continent, especially in late winter to spring seasons when winter monsoon overwhelms the regional transport and mixing of air masses Chao et al.