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Shaw Chen Liu

Researcher at Academia Sinica

Publications -  162
Citations -  12411

Shaw Chen Liu is an academic researcher from Academia Sinica. The author has contributed to research in topics: Ozone & Troposphere. The author has an hindex of 63, co-authored 152 publications receiving 11732 citations. Previous affiliations of Shaw Chen Liu include Georgia Institute of Technology & Northcentral University.

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Ozone production in the rural troposphere and the implications for regional and global ozone distributions

TL;DR: The relationship between O3 and NOx (NO + NO2) which was measured during summer and winter periods at Niwot Ridge, Colorado, has been analyzed and compared to model calculations.
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Case study of the effects of atmospheric aerosols and regional haze on agriculture: an opportunity to enhance crop yields in China through emission controls?

TL;DR: Radiative transfer calculations suggest that regional haze in China is currently depressing optimal yields of approximately 70% of the crops grown in China by at least 5-30%, which could potentially result in a significant increase in crop yields and help the nation meet its growing food demands in the coming decades.
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On the nonlinearity of the tropospheric ozone production

TL;DR: In this article, the relationship of photochemical ozone production versus photochemical loss of an ozone precursor, that is, either NOx or nonmethane hydrocarbons (NMHCs), was studied by using a box model with particular emphasis on the nonlinearity problem of the relationship with respect to the concentration of the precursor.
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Tropospheric ozone : the role of transport.

TL;DR: In this paper, the authors compared the results of the Geophysical Fluid Dynamics Laboratory general circulation/transport model with available observations and found that large-scale atmospheric transport plays a major role in the behavior of tropospheric ozone.
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Potential impact of iodine on tropospheric levels of ozone and other critical oxidants

TL;DR: In this article, the first ever observations of CH3I in the middle and upper free troposphere as recorded during the NASA Pacific Exploratory Mission in the western Pacific were used.