Abstract

Under the National Aeronautics and Space Administration’s (NASA) Making Earth System Data Records for Use in Research Environments (MEaSUREs) Land Surface Temperature and Emissivity project, a new global land surface emissivity dataset has been produced by the University of Wisconsin–Madison Space Science and Engineering Center and NASA’s Jet Propulsion Laboratory (JPL). This new dataset termed the Combined ASTER MODIS Emissivity over Land (CAMEL), is created by the merging of the UW–Madison MODIS baseline-fit emissivity dataset (UWIREMIS) and JPL’s ASTER Global Emissivity Dataset v4 (GEDv4). CAMEL consists of a monthly, 0.05° resolution emissivity for 13 hinge points within the 3.6–14.3 µm region and is extended to 417 infrared spectral channels using a principal component regression approach. An uncertainty product is provided for the 13 hinge point emissivities by combining temporal, spatial, and algorithm variability as part of a total uncertainty estimate. Part 1 of this paper series describes the methodology for creating the CAMEL emissivity product and the corresponding high spectral resolution algorithm. This paper, Part 2 of the series, details the methodology of the CAMEL uncertainty calculation and provides an assessment of the CAMEL emissivity product through comparisons with (1) ground site lab measurements; (2) a long-term Infrared Atmospheric Sounding Interferometer (IASI) emissivity dataset derived from 8 years of data; and (3) forward-modeled IASI brightness temperatures using the Radiative Transfer for TOVS (RTTOV) radiative transfer model. Global monthly results are shown for different seasons and International Geosphere-Biosphere Programme land classifications, and case study examples are shown for locations with different land surface types.

Highlights

  • Infrared land surface emissivity is an important variable in the estimation of Earth’s radiation budget as well as in the retrieval of temperature, water vapor, and other atmospheric constituent profiles from hyperspectral infrared sounders

  • When uncertainties are made available for the Moderate Resolution Imaging Spectroradiometer (MODIS) emissivity, which is intended for the future MOD21 version, it is planned to include these in combination with the currently available ASTER uncertainties in the Combined ASTER and MODIS Emissivity over Land (CAMEL) uncertainty estimates

  • The associated CAMEL quality flag, defined in Table 3, is shown in Figure 1 and shows where no CAMEL emissivity values are reported over sea/inland water, where the input University of Wisconsin–Madison (UW) baseline-fit emissivity dataset (BF) and ASTER data are good quality, the input University of Wisconsin Baseline-Fit (UW BF) is good quality and ASTER is filled, the input UW BF is filled but ASTER is good quality, and both the UW BF and ASTER values are filled

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Summary

Introduction

Infrared land surface emissivity is an important variable in the estimation of Earth’s radiation budget as well as in the retrieval of temperature, water vapor, and other atmospheric constituent profiles from hyperspectral infrared sounders. Under the National Aeronautics and Space Administration’s (NASA) Making Earth System Data Records for Use in Research Environments (MEaSUREs) project, a new and improved global land surface emissivity dataset is being made available. This new dataset, termed the Combined ASTER and MODIS Emissivity over Land (CAMEL), combines previously existing satellite emissivity datasets—those from the Moderate Resolution Imaging Spectroradiometer (MODIS) baseline-fit emissivity dataset (BF) developed at the University of Wisconsin–Madison (UW) [1], and the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) Global Emissivity Dataset v4 (GEDv4) produced at the Jet Propulsion Laboratory (JPL) [2]. The CAMEL uncertainty products, which are discussed in greater detail in this paper, are available at the NASA Land Processes Distributed Active Archive Center (LP DAAC) website

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