Tempestas Radar Turris

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Tempestas radar turris est genus meteorologicum radar, quod est principale instrumentum ad tempestatem convectivam et vigilantiam et admonitionem validam. Eius operandi principium est emittere seriem pulsus electromagneticorum fluctuum, utendo discursum et effusionem fluctuum electromagneticorum per particulas praecipitationes, ut nubes, nebulas, pluvias et nives, ad detectionem spatii distributionis et structurae verticalis praecipitationis, et usus. id ut admonitio et ratio sequi praecipitatio.

Weather radar is mostly pulse radar, which emits short duration (0.25-4 microseconds) pulse waves with a certain repetition rate, and then receives echo pulses scattered by precipitation particles. The scattering and absorption of radar emitted waves by precipitation are related to characteristics such as raindrop spectrum, rainfall intensity, phase state of precipitation particles, shape and orientation of ice crystal particles (see microwave scattering of clouds and precipitation particles, microwave absorption of clouds and precipitation particles). Therefore, analyzing and judging precipitation echoes can determine various macroscopic and microphysical characteristics of precipitation. Various theoretical and empirical relationships have been established between precipitation echo power and precipitation intensity. By utilizing these relationships, the distribution of precipitation intensity and total precipitation within the radar detection range can be determined based on echo power (see Radar Measurement of Precipitation).

Tempestas radar consistit in his elementis fundamentalibus: transfusor - generans pulsus summus frequentiae, antennae directionales - pulsus detectio transmittendi et recipiendi pulsus resonare, recipiens - amplificatio pulsus resonans significationibus, ostensio - ostensio positionis, echo intensio, structura scutorum meteorologicorum ( ut areas praecipitationis et procellae) ad terunt relativum.