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H. L. Miller

Researcher at National Oceanic and Atmospheric Administration

Publications -  16
Citations -  33233

H. L. Miller is an academic researcher from National Oceanic and Atmospheric Administration. The author has contributed to research in topics: Ozone depletion & Absorption (electromagnetic radiation). The author has an hindex of 12, co-authored 16 publications receiving 29523 citations. Previous affiliations of H. L. Miller include Cooperative Institute for Research in Environmental Sciences & University of Colorado Boulder.

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Climate change 2007: the physical science basis

TL;DR: The first volume of the IPCC's Fourth Assessment Report as mentioned in this paper was published in 2007 and covers several topics including the extensive range of observations now available for the atmosphere and surface, changes in sea level, assesses the paleoclimatic perspective, climate change causes both natural and anthropogenic, and climate models for projections of global climate.
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Visible and near‐ultraviolet spectroscopy at McMurdo Station, Antarctica: 9. Observations of OClO from April to October 1991

TL;DR: In this paper, a series of measurements of atmospheric OClO covering the period April to October 1991, made at McMurdo Station, Antarctica, were made to extend the knowledge of the general role of atmospheric chlorine dioxide in the general problem of ozone depletion.
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Visible and near‐ultraviolet spectroscopy at McMurdo Station, Antarctica 7. OClO diurnal photochemistry and implications for ozone destruction

TL;DR: In this paper, observations of the ratio between the change in slant column abundance of OClO and ozone as a function of solar zenith were used to deduce the diurnal cycle of the daytime ozone column abundance above Antarctica during September 1987.
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Atmospheric NO3: 1. Measurement technique and the annual cycle at 40°N

TL;DR: In this paper, the authors show that the NO3 absorption feature has strong negative correlation with water vapor, which requires that water vapor absorption be explicitly considered in attempts to measure NO3 from the ground.
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Retrieving cloud information from passive measurements of solar radiation absorbed by molecular oxygen and O2-O2

TL;DR: In this article, the ability to retrieve key information about clouds from observations of atmospheric absorption by molecular oxygen along with the O2-O2 collision complex is examined, and the authors demonstrate through theoretical calculations that these cloud parameters can be accurately retrieved from measurements of fractional absorption at moderate resolution and with no requirement of absolutely calibrated radiances.