Spatiotemporal High-Resolution Cloud Mapping with a Ground-Based IR Scanner

<div>Scatterplot NubiScope internal temperature versus residual radiance (NubiScope measurement minus Streamer modelled spectral radiance) at a zenith angle of 3°. Solid line represents linear regression model of all points taken into account, dashed line is regression line plus two standard deviations of the residual radiance, and formula and <svg height="11.7978pt" id="M13" style="vertical-align:-0.2063999pt" version="1.1" viewbox="-0.0498162 -11.5914 10.5526 11.7978" width="10.5526pt" xmlns="http://www.w3.org/2000/svg" xmlns:xlink="http://www.w3.org/1999/xlink"><g transform="matrix(.013,0,0,-0.013,0,0)"><path d="M393 379C402 394 400 411 393 422C384 437 365 448 348 448C301 448 237 372 186 285H182L193 335C210 408 205 448 178 448C150 448 80 402 29 344L45 321C80 355 114 373 122 373C128 373 130 365 124 330C106 228 76 98 50 -5L57 -12C82 -5 112 3 132 6L172 203C196 256 234 304 254 329C275 355 293 367 306 367C318 367 330 360 342 348C347 343 355 343 365 350S386 367 393 379Z" id="g113-115"></path></g><g transform="matrix(.0091,0,0,-0.0091,5.488,-5.741)"><path d="M414 144C384 79 371 75 317 75H135L276 221C367 316 408 376 408 465C408 570 327 635 237 635C179 635 131 609 100 575L42 494L67 471C94 510 138 565 205 565C277 565 321 517 321 435C321 348 258 270 195 195C146 137 88 81 33 26V0H411C423 44 433 88 446 135L414 144Z" id="g50-51"></path></g></svg> belong to the regression model.</div>

Advances in Meteorology

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Figure 2

Figure 2: Spatiotemporal High-Resolution Cloud Mapping with a Ground-Based IR Scanner 