The Marine-Atmospheric Emitted Radiance Interferometer: A High-Accuracy, Seagoing Infrared Spectroradiometer
Open Access
- 1 June 2001
- journal article
- Published by American Meteorological Society in Journal of Atmospheric and Oceanic Technology
- Vol. 18 (6), 994-1013
- https://doi.org/10.1175/1520-0426(2001)018<0994:tmaeri>2.0.co;2
Abstract
The Marine-Atmospheric Emitted Radiance Interferometer (M-AERI) is described, and some examples of the environmental variables that can be derived from its measurements and the types of research that these can support are briefly presented. The M-AERI is a robust, accurate, self-calibrating, seagoing Fourier-transform interferometric infrared spectroradiometer that is deployed on marine platforms to measure the emission spectra from the sea surface and marine atmosphere. The instrument works continuously under computer control and functions well under a very wide range of environmental conditions with a high rate of data return. Spectral measurements are made in the range of ∼3 to ∼18 μm wavelength and are calibrated using two internal, National Institute of Standards and Technology–traceable blackbody cavities. The environmental variables derived from the spectra include the surface skin temperature of the ocean, surface emissivity, near-surface air temperature, and profiles of temperature and h... Abstract The Marine-Atmospheric Emitted Radiance Interferometer (M-AERI) is described, and some examples of the environmental variables that can be derived from its measurements and the types of research that these can support are briefly presented. The M-AERI is a robust, accurate, self-calibrating, seagoing Fourier-transform interferometric infrared spectroradiometer that is deployed on marine platforms to measure the emission spectra from the sea surface and marine atmosphere. The instrument works continuously under computer control and functions well under a very wide range of environmental conditions with a high rate of data return. Spectral measurements are made in the range of ∼3 to ∼18 μm wavelength and are calibrated using two internal, National Institute of Standards and Technology–traceable blackbody cavities. The environmental variables derived from the spectra include the surface skin temperature of the ocean, surface emissivity, near-surface air temperature, and profiles of temperature and h...Keywords
This publication has 21 references indexed in Scilit:
- An Independent Assessment of Pathfinder AVHRR Sea Surface Temperature Accuracy Using the Marine Atmosphere Emitted Radiance Interferometer (MAERI)Bulletin of the American Meteorological Society, 2000
- Meteorological Applications of Temperature and Water Vapor Retrievals from the Ground-Based Atmospheric Emitted Radiance Interferometer (AERI)Journal of Applied Meteorology and Climatology, 1998
- An overview of MODIS capabilities for ocean science observationsIEEE Transactions on Geoscience and Remote Sensing, 1998
- Observations of the oceanic thermal skin in the Atlantic OceanJournal of Geophysical Research: Oceans, 1997
- A Third Generation Water Bath Based Blackbody SourceJournal of Research of the National Institute of Standards and Technology, 1995
- STEP—A Temperature Profiler for Measuring the Oceanic Thermal Boundary Layer at the Ocean–Air InterfaceJournal of Atmospheric and Oceanic Technology, 1990
- Emissivity of pure and sea waters for the model sea surface in the infrared window regionsRemote Sensing of Environment, 1988
- Heat thermal structure in the interfacial boundary layer measured in an open tank of water in turbulent free convectionJournal of Fluid Mechanics, 1977
- Infrared Characteristics of Ocean Water (15 –15 μ)Applied Optics, 1969
- Heat transfer in the top millimeter of the oceanJournal of Geophysical Research, 1969