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Patrones de calentamiento superficial y clima

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Patrones de calentamiento superficial y clima

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About this activity

Calentamiento superficial y clima.

Created by

MARITZA NATHALY CHALCO JARAMILLO
MARITZA NATHALY CHALCO JARAMILLO
Ecuador

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Patrones de calentamiento superficial y clima
 

Patrones de calentamiento superficial y climaOnline version

Calentamiento superficial y clima.

by MARITZA NATHALY CHALCO JARAMILLO
1

Introducción al calentamiento superficial

El calentamiento de la superficie varía con el sol, el suelo y el agua, creando diferencias de temperatura locales.

2

Factores que calientan la superficie

Factores clave: sol directo, albedo (reflexión), humedad y capas superficiales del suelo.

3

Formación de vientos

Las diferencias de temperatura generan gradientes de presión, impulsando movimientos de aire y la formación de vientos.

4

Vientos locales

En relieve, el calentamiento desigual produce vientos locales como brisas de valle y de montaña.

5

Convección y nubes

El aire caliente asciende por convección, formándose nubes cuando la humedad se condensa.

6

Nubes y tormentas

La convección continúa alimentando la formación de nubes cumuliformes y tormentas en zonas cálidas.

7

Precipitación

La nubosidad y la evaporación favorecen la precipitación cuando las gotas crecen y caen como lluvia.

8

Presión y sistemas climáticos

El calentamiento desigual genera sistemas de baja presión que distribuyen lluvia y vientos a gran escala.

9

Ciclo diario y clima local

El calentamiento diario cambia la humedad y la intensidad de los vientos, influyendo en la lluvia local.

10

Conceptos clave

Resumen: el calentamiento de la superficie crea vientos, nubes y lluvias interconectados por convección y presión.
 
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