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atmosphereArticleComparisons involving Mean and Turbulent Parameters of AircraftBased and ShipBased Measurements inside the Marine Atmospheric Boundary LayerMinSeong Kim 1 , Byung Hyuk Kwon 2, and TaeYoung GooConvergence Meteorological Investigation Department Aviation Observation Research Team, National Institute of Meteorological Sciences, Seogwipo 63568, Jejudo, Korea; [email protected] (M.S.K.); [email protected] (T.Y.G.) Department of Environmental Atmospheric Sciences, Pukyong National University, Busan 48513, Gyeongsangnamdo, Korea Correspondence: [email protected]: Kim, M.S.; Kwon, B.H.; Goo, T.Y. Comparisons in between Imply and Turbulent Parameters of AircraftBased and ShipBased Measurements inside the Marine Atmospheric Boundary Layer. Atmosphere 2021, 12, 1088. https:// doi.org/10.3390/atmos12091088 Academic Editors: Zhenru Shu, PakWai Chan and Yuncheng He Received: 15 June 2021 Accepted: 20 August 2021 Published: 24 AugustAbstract: The Structure des Echanges MerAtmosph e, Propri Oc niques/ Recherche Exp imentale (SEMAPHORE) experiment was conducted over the oceanic Azores present situated inside the Azores Basin. The evolution of your marine atmospheric boundary layer (MABL) was studied based on the evaluation of mean and turbulent data employing in situ measurements by a ship and two aircrafts. The sea surface temperature (SST) field was characterized by a gradient of about 1 C/100 km. The SST measured by aircraft decreased at a ratio of 0.25 C/100 m of altitude on account of the divergence from the infrared radiation flux from the surface. With the exception of temperature, the mean parameters measured by the two aircrafts were in superior agreement with every single other. The sensible heat flux was more dispersed than the latent heat flux in accordance with the comparisons involving aircraft and aircraft, and aircraft and ship. This study demonstrates the feasibility of applying two aircraft to describe the MABL and surface flux with confidence. Keywords: marine atmospheric boundary layer; sea surface temperature; infrared flux divergence; heat flux; SEMAPHORE1. Introduction The determination of boundary layer conditions in the air cean interface is an vital concern in atmospheric and oceanic predictive numerical models. The air ea exchanges of momentum, heat, and water are substantial in atmospheric and oceanic movements at diverse scales. Accurate Niaprazine Histamine Receptor predictions of complicated and poorly understood marine environments need an improved understanding of spatial variability and highly precise parameterization of turbulent surface flows [1]. The atmospheric turbulent fluxes of heat, water vapor, and momentum across the air cean interface play a substantial role within the development of climate and the climate technique. As a result, they must be an integral aspect of numerical weather prediction and climate prediction models. Mainly because this exchange is mainly in the subgrid scale, it is parameterized by a surface bulk exchange parameterization scheme which is semiempirical. Abundant intensive observations of turbulent exchange are required to improve the algorithm, ordinarily by estimating the exchange coefficients [2,3]. Interactions in between the ocean and atmosphere have been experimentally studied from turbulence to synoptic scales for various years. 7-TFA-ap-7-Deaza-dA Biological Activity Several on the connected research focused around the examination of physical processes in the marine a.
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