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4S - SILVERSWORD SOFTWARE AND SERVICES, LLC STTR Phase I Award, June 2022

A STTR Phase I contract was awarded to 4S - Silversword Software And Services, Llc in June, 2022 for $139,786.0 USD from the U.S. Department of Defense and United States Navy.

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Contents

sbir.gov/node/2237575
Is a
SBIR/STTR Awards
SBIR/STTR Awards

SBIR/STTR Award attributes

SBIR/STTR Award Recipient
4S - Silversword Software And Services, Llc
4S - Silversword Software And Services, Llc
0
Government Agency
U.S. Department of Defense
U.S. Department of Defense
0
Government Branch
United States Navy
United States Navy
0
Award Type
STTR0
Contract Number (US Government)
N68335-22-C-03000
Award Phase
Phase I0
Award Amount (USD)
139,7860
Date Awarded
June 6, 2022
0
End Date
December 6, 2022
0
Abstract

The Planetary Boundary Layer (PBL) is the layer of atmosphere bordering the surface of the earth and represents the greatest importance to human activities. It is also the most difficult layer of the atmosphere to measure directly. These dual properties of high importance yet difficulty of measurement have led some people in the atmospheric profiling community to call a space-based measurement approach to a complete profile of PBL properties the Holy Grail of atmospheric profiling. In recent years it has received tremendous attention given the importance and difficulty of the problem. According to the NASA PBL Incubation Study Team Report: “A global Planetary Boundary Layer (PBL) observing system is urgently needed to address fundamental PBL science questions and societal applications related to weather, climate, and air quality” [Teixeira, J. et al, 2021]. In addition to the needs outlined in the report, 4S experience in developing Free Space Optical Communication (FSOC) devices under contract from NAVAIR has led to an understanding that the technology stands to benefit from high resolution models and forecasts to predict atmospheric conditions that degrade laser beam quality. The Marine Atmospheric Boundary Layer (MABL) has greater complications with high variability over a wide range of temporal and spatial scales due to high horizontal heterogeneity introduced by mesoscale ocean phenomena. Additionally, in situ observations of the MABL are sparse when compared to land based in situ observations. A complete observational approach that accounts for the ocean, the MABL thermodynamic structure, and clouds is required to properly profile the MABL.

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