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Relative humidity is an important metric used in weather forecasts and reports, as it is an indicator of the likelihood of precipitation, dew, or fog. In hot summer weather, a rise in relative humidity increases the apparent temperature to humans (and other animals) by hindering the evaporation of perspiration from the skin.
"When you go home tell them of us and say: for your tomorrow we gave our today" inscribed on a war memorial in Westbury-on-Trym. Edmonds is credited with authorship of a famous epitaph in the War Cemetery in Kohima which commemorates the fallen of the Battle of Kohima in April 1944.
"The Good-Morrow" is a poem by John Donne, published in his 1633 collection Songs and Sonnets. Written while Donne was a student at Lincoln's Inn , the poem is one of his earliest works and is thematically considered to be the "first" work in Songs and Sonnets .
The simplest method of forecasting the weather, persistence, relies upon today's conditions to forecast tomorrow's. This can be valid when the weather achieves a steady state, such as during the summer season in the tropics. This method strongly depends upon the presence of a stagnant weather pattern.
Apparent temperature, also known as "feels like", [1] [2] is the temperature equivalent perceived by humans, caused by the combined effects of air temperature, relative humidity and wind speed. The measure is most commonly applied to the perceived outdoor temperature.
For a constant temperature, the smaller the difference, the more moisture there is, and the higher the relative humidity. In the lower troposphere, more moisture (small dew point depression) results in lower cloud bases and lifted condensation levels (LCL). LCL height is an important factor modulating severe thunderstorms.
Cumulus humilis indicates a dry day ahead.. Weather lore is the body of informal folklore related to the prediction of the weather and its greater meaning.. Much like regular folklore, weather lore is passed down through speech and writing from normal people without the use of external measuring instruments.
It is based on the reddish glow of the morning or evening sky, caused by trapped particles scattering the blue light from the sun in a stable air mass. [5] If the morning skies are of an orange-red glow, it signifies a high-pressure air mass with stable air trapping particles, like dust, which scatters the sun's blue light.