The project was conducted during July and August 1991 under low vertical wind shear situations. The initiation, organization, and longevity of thunderstorms associated with boundary layer convergence lines in the Cape Canaveral, Florida, vicinity are examined using data from the Convection and Precipitation/Electrification (CaPE) experiment. Thermal internal boundary layer, and turbulent mixing are also Some boundary-layerĬharacteristics needed for predicting diffusion of pollutants releasedįrom coastal launch pads, including atmospheric stability, depth of the Time, strength, depth, propagation speed and both landward and seawardĮxtension, are documented in this study. Detailed characteristics over aĭiurnal cycle of the sea-land breeze and of the river breeze onset Rotation rate suggests that mesoscale forcing significantly modifies theĬoriolis-induced oscillation. The nighttime flow structure was dominated by a large-scale landīreeze that was relatively uniform over the area and became In the surrounding areas and speeding up the movement of the sea-breezeįront. The rivers near theĬoastline also modified the initial flow field by enhancing convergence The sea-breeze convergence on the seaward side and generated additionalĬonvergence on the landward side of the river. The Indian River breeze, in that divergent flow over the river enhanced A strong sea-breeze circulation, the dominant feature of theĭaytime flow field, was modified by a local inland river breeze known as Pressure-gradient form created by the temperature contrast between landĪnd water.
Theĭaytime flow structure was determined primarily by the mesoscale Inland rivers) occurs and the local circulations are most intense.
Greatest daytime temperature difference between land and water (sea and The case wasĬhosen from the spring intensive data-collection period when the Space Center Atmospheric Boundary Layer Experiment (KABLE). The diurnal evolution of the three-dimensional structure of a mesoscaleĬirculation system frequently occurring in the area of Kennedy SpanĬenter-Cape Canaveral has been studied using the data from the Kennedy Utilities derived from this climatology were developed to assist forecasters in determining the land-breeze occurrence, timing, and movement based on predicted meteorological conditions. Five-minute observations of winds, temperature, and moisture along with 9 15-MHz Doppler Radar Wind Profiler data were used to analyze specific land-breeze cases, while the tower data were used to construct a composite climatology. This comprehensive analysis was enabled by the high-resolution tower observations over KSC/CCAFS. This report presents a seven-year observational study of land breezes over east-central Florida from 1995 to 2001. Accurate predictions of the land breeze are critical for toxic material dispersion forecasts associated with space launch missions, since wind direction and low-level stability can change noticeably with the onset of a land breeze. The occurrence and timing of land breezes impact low-level winds, atmospheric stability, low temperatures, and fog development. Review on the past lesson Please pass your assignments in the count of 5 4 3 2 1.The nocturnal land breeze at the Kennedy Space Center (KSC) and Cape Canaveral Air Force Station (CCAFS) is both operationally significant and challenging to forecast. Good morning Ma’am (prayer) Great ma’am B. Those who are not in their seats will be marked absent.
Preliminary Activity Good morning class Please stand for our prayer to be lead by Ariel. PROCEDURE Teacher’s Activity Student’s Activity A. Values Integration Collaboration, cooperation, teamwork F. Instructional Materials: Visual aids, pictures, illustration, manila paper. References: Science Grade 7 Learner’s Material Module C. Point out the difference between land breeze and sea breeze. Explain how land breeze and sea breeze occur. OBJECTIVES At the end of the lesson, the learners will be able to: 1. A Detailed Lesson Plan In Science for Grade 7 Students Prepared by: Kristine Ann L.
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