Describe how the summer monsoons affects the living conditions of people and the production of food in india

hola:

ef0: daños leves. algunas tejas caídas y otras pequeñas piezas de los tejados arrancadas, algunos daños en canaletas, ramas de árboles rotas y algunos árboles poco profundos arrancados. los tornados que no causan daños visibles (por ejemplo aquellos que se producen en campos abiertos) se valoran siempre como de ef0.

ef1: daños moderados. tejados seriamente despedazados, caravanas y casetas volcadas o seriamente dañadas, perdida de puertas exteriores y ventanas y otros cristales rotos.

ef5: daños increíbles. las casas fuertes pueden quedar arrasadas hasta los cimientos, las estructuras de hormigón armado dañadas críticamente, los edificios altos sufren graves deformaciones estructurales. devastaciones increíbles.

y según esto creo que puedes sacar tus conclusiones. y la verdad la escala ef10 si no se decirte por que no la eh visto o mejor dicho estudiado. espero que te sirva. suerte.

explanation:

high and low pressure systems produce opposing weather conditions. high pressure systems are generally associated with fair weather, while low pressure systems bring clouds, precipitation and sometimes stormy conditions.

fair vs. stormy conditions

high and low pressure systems produce opposing weather conditions. high pressure systems are generally associated with fair weather, while low pressure systems bring clouds, precipitation and sometimes stormy conditions. while just sunshine and fair-weather clouds typically accompany high pressure systems, a range of conditions, ranging from mild drizzle to heavy snow to intense lightening, occur under areas of low pressure. additionally, high pressure systems usually produce only light winds, while the storminess associated with low pressure systems can produce strong, sometimes even damaging winds.

sinking vs. rising air

high pressure systems entail sinking air, while lows entail rising air. high pressure systems form where air converges in the higher levels of the atmosphere. the converging air has nowhere to go and is forced to sink toward the ground. this sinking effect inhibits cloud formation and therefore precipitation. in contrast, low pressure systems form where air near the ground converges. with no place else to go, it rises. in doing so, water vapor cools and condenses into tiny water droplets or ice crystals, producing clouds and precipitation.

clockwise vs. counterclockwise wind flow

due to the rotation of the earth -- precisely, the coriolis effect -- winds spiral around high and low pressure systems in a circular pattern. but they do so in opposite directions, and these directions are reversed in the earth’s two hemispheres. in high pressure systems, the air flows clockwise in the northern hemisphere and counterclockwise in the southern hemisphere. with low pressure systems, winds blow counterclockwise in the northern hemisphere and clockwise in the southern hemisphere.