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PRecursore IperSpettrale della Missione Applicativa (PRISMA, Candela et al.,Дў016), which provides similar spectral range and Of present missions, this analysis may be applicable to the Italian Requirements Document refers repeatedly to О” x<30вЂ‰m The prime contractor was selected in July 2020 and whose Mission О” x of 30вЂ“60вЂ‰m, and for ESA's Copernicus Hyperspectral Imaging Mission for the Environment (CHIME), also known as Sentinel 10, for which (HysPIRI, Lee et al., 2015) concept offering (SBG) designated observable, with the Hyperspectral Infrared Imager However, similar or improvedД¬apacity is anticipated in response to NASA's Surface Biology and Geology Station (ISS) in 2022 with an average footprint size ( О” x) of 60вЂ‰m (Green and Thompson, 2020). WeДЇocus on the EMIT mission, planned to launch to the International Space Hyperspectral VSWIR measurement capacity at fine horizontal resolution. This study is primarily motivated by the ongoing development of spaceborne

Measurement gap using upcoming observations from very high-spatial-resolution visible and shortwave infrared reflectance (VSWIR) observations from space. This paper will address the feasibility of addressing this Global scale to evaluate the small-scale variability produced by these Higher-order closure approaches that include prognostic equations for higher-order moments such as the variance (GolazД®t al., 2002 Larson et al., 2002). Modern approaches to parameterise PBL variability include eddy-diffusivity/mass-flux approaches (Suselj et al., 2019) and Spatial variability of q v is not resolved by current global weather orД¬limate models, but instead it must be parameterised. Furthermore, in situ observations suggest that the majority of the variation in the TCWV prior to convective initiation can be Mesoscale aggregation in PBL water vapour appears to play an important role in determining the timing of deep convective events Thermodynamics is the inability to quantify mesoscale variations in PBL A critical measurement gap in the current observations of PBL Layer clouds was also highlighted due to their importance for Earth's energyД«alance.

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вЂњliterally couples the surface of the Earth to the atmosphere aboveвЂќ, and among other important factors, gradients of moisture between the surface and PBL and between the PBL and free troposphere are strong controls on vertical atmospheric heat and moisture transport. TheДecadal Survey explicitly recognised the PBL's importance since it PBL q v estimates would go beyond theД¬urrent total column water vapour (TCWV) and free-tropopause products to provide new information about the vertical moisture structure for weather and climate applications. Recommended by NASA's Decadal Survey (National Academies of Science, Engineering, and Medicine, 2018). Including information about water vapour ( q v), is a targeted observable Thermodynamic information about the planetary boundary layer (PBL), Offer new information on PBL water vapour spatial statistics to the VSWIR instruments, primarily targeting surface properties, can therefore

The true histograms of TCWV at the nominal footprint resolution. However, the derived histograms of TCWV in an area are closely related to Obtained by current sensors, the derived maps correspond poorly to true TCWVДЄt the pixel scale, with r 2<0.6 at SZA = 30 в€. Even at the 250вЂ‰m horizontal resolution regularly Finally, we account for changing solar zenith angle (SZA) fromДЎ5 to 60 в€ and show that the non-vertical solar path destroys the correspondence between footprint-retrieved TCWV and the true TCWV directlyДЄbove that footprint. Future retrieval development could greatly mitigate Standard deviation and are primarily related to the retrieval's assumedДЄtmospheric profiles. Removed, but biases from в€’7вЂ‰% to +34вЂ‰% remain in retrieved spatial Random retrieval errors are easily quantified and That the domain surface is uniformly composed of either vegetated surfaces Using an observing system simulationД®xperiment (OSSE) applied to large eddy simulation (LES) output, we show that EMIT can retrieve horizontal variability in PBL water vapour, provided We provide evidence that for convective planetaryД«oundary layers (PBLs), spatial variability in TCWV corresponds to Measurements, and modern missions such as the upcoming Earth Surface MineralДust Source Investigation (EMIT) offer unprecedented horizontal resolution Daytime clear-sky total column water vapour (TCWV) isД¬ommonly retrieved from visible and shortwave infrared reflectance (VSWIR)

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