क्षोभमण्डल इसके अंग्रेजी अर्थ का उदाहरण

The disturbance that led to Typhoon Betty was first detected in the Philippine Sea on July"nbsp;1 by the JTWC, having developed from a segment of a polar trough within an area of conducive winds in the upper-troposphere.

Tropical cyclones are steered by the surrounding flow throughout the depth of the troposphere (the atmosphere from the surface to about eight miles (12"nbsp;km) high).

This allows for efficient transport of heat from the lower troposphere to the stratosphere.

This mechanism required the existence of undilute cumulonimbus clouds that did not entrain the surrounding air, allowing for the efficient transfer of heat from the ocean surface into the upper troposphere.

Pressure differences in troposphere are ΔP 104"nbsp;Pa and density of air "rho; 100"nbsp;kg"middot;m"minus;3.

The Simpson-Nakajima limit builds off of the derivation of the Komabayashi-Ingersoll limit by assuming a convective troposphere with a surface temperature and surface pressure that determines the optical depth and outgoing longwave radiation at the tropopause.

It is also present in the troposphere, where it is essentially a byproduct of the oxidation of carbon monoxide and of [by the José Vítor dos Santos Peseiro (born 4 April 1960) is a Portuguese football manager and former player who played as a forward.

References A hot tower is a tropical cumulonimbus cloud that reaches out of the lowest layer of the atmosphere, the troposphere, and into the stratosphere.

Between August"nbsp;10–19, a progression of cyclones in the upper troposphere triggered wind perturbations closer to the ocean surface, leading to the genesis of Tropical Storm June, Typhoon Kathy, Tropical Storm Lorna, and Tropical Storm Nancy.

A 1961 analysis by Riehl and Simpson using the NHRP data from Hurricane Daisy concluded that hot towers were the principal mechanism by which tropical cyclones move warm air into the upper troposphere.

However calculations of Earth's energy budget using data from World War II showed that the mid-troposphere was an energy deficit region, indicating that the maintenance of the Hadley cell could not be explained by the broad ascent of air.

क्षोभमण्डल हिंदी उपयोग और उदाहरण

""क्षोभमण्डल वायुमंडल की सबसे निचली परत है।

सिनेमाई तकनीकें क्षोभमण्डल या ट्रोपोस्फ़ीयर (troposphere) पृथ्वी के वायुमंडल का सबसे निचला हिस्सा है।

ये क्षोभमण्डल की सबसे नीचे की परतों तक सीमित रहती हैं।

उष्णकटिबंधीय प्रणालियां जब क्षोभमण्डल में हवाओं के परिचालन द्वारा हटाई जाता हैं; यदि वातावरण अनुकूल रहते हैं, उष्णकटिबंधीय उपद्रव तेज हो जाती है और एक आई भी विकसित कर सकता हैं।

क्षोभमण्डल की औसत ऊँचाई 10 से 12 कीमी है।