Abstract

We present the project of a 2U CubeSat format spaceborne multichannel laser heterodyne spectroradiometer (MLHS) for studies of the Earth’s atmosphere upper layers in the near-infrared (NIR) spectral range (1258, 1528, and 1640 nm). A spaceborne MLHS operating in the solar occultation mode onboard CubeSat platform, is capable of simultaneous vertical profiling of CO2, H2O, CH4, and O2, as well as Doppler wind measurements, in the tangent heights range of 5–50 km. We considered the low Earth orbit for the MLHS deployment and analyzed the expected surface coverage and spatial resolution during one year of operations. A ground-based prototype of the MLHS for CO2 and CH4 molecular absorption measurements with an ultra-high spectral resolution of 0.0013 cm−1 is presented along with the detailed description of its analytical characteristics and capabilities. Implementation of a multichannel configuration of the heterodyne receiver (four receivers per one spectral channel) provides a significant improvement of the signal-to-noise ratio with the reasonable exposure time typical for observations in the solar occultation mode. Finally, the capability of building up a tomographic picture of sounded gas concentration distributions provided by high spectral resolution is discussed.

Highlights

  • The recent development of carbon balance instrumental control technology is aimed at, but not limited to, highly accurate evaluation of sources and sinks of major greenhouse gases (GHG) by natural landscapes, cities, industrial and agricultural objects

  • Solar radiation for each intermediate frequency (IF) receiver is delivered by fiber bundle (FB); its spectral channel, one fiber collimator (FCol) is used

  • Exploiting FB allows decreasing the weight of ber bundle (FB); its structure is presented in Figure 12a as well

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Summary

Introduction

The recent development of carbon balance instrumental control technology is aimed at, but not limited to, highly accurate evaluation of sources and sinks of major greenhouse gases (GHG) by natural landscapes, cities, industrial and agricultural objects. Precise measurements of GHG distribution in the atmosphere with global coverage and sufficient spatial and temporal resolution may facilitate the characterization of carbon balance at the macroregional level [1]. As the role of particular natural systems in such a balance may evolve following climate change, it is essential to provide continuous monitoring with sufficient spatial and temporal resolution. One way to improve the characterization of carbon dioxide atmospheric transport is its precise vertical profiling which, along with detailed mapping provided by the existing and future spaceborne instruments, may efficiently augment the datasets employed in global carbon balance models

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