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  1. Hace 3 días · Hint: We have given the angle of elevation cloud from the point \[200{\text{ }}metres\]above the lake is \[{30^o}\]an angle of depression is of reflection of the cloud is \[{60^o}\].So, firstly we have to draw a rough diagram of the situation. After this, we calculate the base length. This base length helps us to find the height of the cloud from the ground level.

  2. Hace 2 días · Description. CER_SYN1deg-3Hour_Terra-MODIS_Edition4A is the Clouds and the Earth's Radiant Energy System (CERES) and geostationary (GEO)-Enhanced Top of Atmosphere (TOA), Within-Atmosphere and Surface Fluxes, Clouds and Aerosols 3-Hourly Terra Edition4A data product, which was collected using Imaging Radiometers on the Geostationary Satellites ...

  3. Hace 5 días · Calcolo base nubi. L'altezza base del cumulo è l'altitudine più bassa della porzione visibile di una nuvola. Può essere misurata usando un ceilometro: un dispositivo che riflette un raggio di luce dalla base della nuvola e calcola la sua distanza usando la triangolazione. In alternativa, la base della nuvola può essere stimata anche ...

  4. Hace 2 días · These formulas have evolved with time, incorporating more variables and factors to increase accuracy. Calculation Formula. The formula to predict the wave height caused by wind is given by: \[ H = k \cdot v^2 \] where: \(H\) is the wave height in meters, \(k\) is the coefficient related to water body characteristics and wind speed,

  5. Hace 2 días · For instance, if someone has a neck circumference of 15 inches and a height of 70 inches, the Neck to Height Ratio would be: \[ \text{Neck to Height Ratio} = \frac{15}{70} = 0.2142857143 \] Importance and Usage Scenarios

  6. Hace 2 días · The cloud properties are averaged for both day and night (24-hour) and day-only time periods. Cloud properties are stratified into 4 atmospheric layers (surface-700 hPa, 700 hPa, - 500 hPa, 500 hPa, - 300 hPa, 300 hPa, - 100 hPa) and a total of all layers.

  7. Hace 2 días · Description. PISTON-ONR-NOAA_RVThompson_2019 is the Propagation of Intra-Seasonal Tropical Oscillations (PISTON) 2018 Research Vessel (RV) Thompson data product. This product is the result of a joint effort that involved NASA as well as the Office of Naval Research (ONR), and National Oceanic and Atmospheric Administration (NOAA).