Absolutely Stable AirAn atmospheric condition that exists when the environmental lapse rate is less than the moist adiabatic lapse rate.
Absolutely Unstable AirAn atmospheric condition that exists when the environmental lapse rate is greater than the dry adiabatic lapse rate.AbsorptionThe process in which incident radiant energy is retained by a substance by conversion to some other form of energy.Automated Surface Observing SystemThe ASOS program is a joint effort of the National Weather Service (NWS), the Federal Aviation Administration (FAA), and the Department of Defense (DOD). Completed in the mid-1990s, the ASOS systems serve as the nation's primary surface weather observing network. ASOS is designed to support weather forecast activities and aviation operations and, at the same time, support the needs of the meteorological, hydrological, and climatological research communities.Bright Surge on the Disk (BSD)In solar-terrestrial terms, a bright gaseous stream (surge) emanating from the chromosphere.Bright Surge on the Limb (BSL)In solar-terrestrial terms, a large gaseous stream (surge) that moves outward more than 0.15 solar radius above the limb.BSBlowing SnowCooperative ObserverAn individual (or institution) who takes precipitation and temperature observations-and in some cases other observations such as river stage, soil temperature, and evaporation-at or near their home, or place of business. Many observers transmit their reports by touch-tone telephone to an NWS computer, and nearly all observers mail monthly reports to the National Climatic Data Center to be archived and published. Dobson UnitUnit used to measure the abundance of ozone in the atmosphere. One Dobson unit is the equivalent of 2.69/ x 1016 molecules of ozone/cm2.EBSEmergency Broadcast SystemOBSObservation(s)OBSCObscureObscurationAny atmospheric phenomenon, except clouds, that restricts vertical visibility (e.g., dust, rain, snow, etc.). Obscuring PhenomenaAny atmospheric phenomenon, except clouds, that restricts vertical visibility (e.g., dust, rain, snow, etc.).Observation WellIn hydrologic terms, a non-pumping well used for observing the elevation of the water table or piezometric surfacePolar Cap Absorption (PCA)In solar-terrestrial terms, an anomalous condition of the polar ionosphere whereby HF and VHF (3 - 300 MHz) radiowaves are absorbed, and LF and VLF (3 - 300 kHz) radiowaves are reflected at lower altitudes than normal. In practice, the absorption is inferred from the proton flux at energies greater than 10 MeV, so that PCAs and
proton events are simultaneous. Transpolar radio paths may still be disturbed for days, up to weeks, following the end of a proton event.Rawinsonde ObservationA radiosonde observation which includes wind data.Remote Observing System AutomationA type of automated data transmitter used by NWS Cooperative Program observers.River Observing StationAn established location along a river designated for observing and measuring properties of the river.SBSDSubsideSubsidence1. A descending motion of air in the atmosphere occurring over a rather broad area.
2. In hydrologic terms, sinking down of part of the earth's crust due to underground excavation, such as the removal of groundwater.Subsidence InversionA temperature inversion that develops aloft as a result of air gradually sinking over a wide area and being warmed by adiabatic compression, usually associated with subtropical high pressure areas.SubstationA location where observations are taken or other services are furnished by people not located at NWS offices who do not need to be certified to take observations.Subsurface Storm FlowIn hydrologic terms, the lateral motion of water through the upper layers until it enters a stream channel. This usually takes longer to reach stream
channels than runoff. This also called interflow.Voluntary Observing Ship Program(VOS) - An international voluntary marine observation program under the auspices of the World Meteorological Organization (WMO). Observations are coded in a special format known as the ships synoptic code, or "BBXX" format. They are then distributed for use by meteorologists in weather forecasting, by oceanographers, ship routing services, fishermen, and many others.
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