Earlier, tropical storms were identified in random ways — by places, objects, or even feast days of saints. But this caused confusion in communication and disaster warnings. 👉 The first systematic step came from Clement Wragg, a Queensland Government Meteorologist (Australia), who used personal names for cyclones between 1887–1907. Today, naming is a formal, scientific,…
General Characteristics When we talk about cyclones, we usually divide them into two big categories: Here, we focus on tropical cyclones. Unlike their temperate counterparts, they are not uniform or regular. Their size, shape, intensity, and impact differ greatly. But still, some general characteristics help us identify them. Let’s go through these one by one….
When we hear the word cyclone, we often imagine massive storms near the equator like hurricanes or typhoons. But in reality, the cyclones that dominate the weather of Europe, North America, and much of Asia are not tropical—they are called temperate cyclones. These are also known as: Basic Nature 👉 In short: Temperate cyclones are…
Suppose you are standing on a vast open plain, feeling the wind rush past you. You notice that the wind doesn’t just blow randomly—it follows patterns shaped by forces far beyond what the eye can see. This is the world of atmospheric circulation, where cyclones and anticyclones play a pivotal role in shaping weather patterns…
Fronts and Frontogenesis Imagine the atmosphere as a huge battlefield where different armies of air are always in motion. These armies are called air masses — large bodies of air that have uniform characteristics like temperature, humidity, and pressure. Now, what happens when two very different air masses face each other? For example: The line…
Imagine you are standing in Rajasthan on a hot summer afternoon — the air feels scorching, dry, and persistent. Now, travel in your mind to the coastal region of Kerala during the monsoon — the air is warm, but moist, heavy with water vapour. Both are examples of air masses — vast bodies of air…
Rainfall is not evenly distributed across the globe. Some regions receive heavy and consistent rain throughout the year, while others remain dry for extended periods. This variation is due to multiple factors such as proximity to the sea, wind direction, mountains, and altitude. Let’s break down the distribution of rainfall worldwide and explore the different…
Imagine you are standing in an open field on a humid afternoon, feeling the air heavy with moisture. Slowly, the wind picks up, and the sky darkens. You sense the inevitable arrival of rain—but what really happens in the sky before those raindrops touch the ground? Let’s take a journey through the science of rainfall,…
Precipitation is nature’s way of delivering water from the atmosphere to the Earth. Imagine warm, moist air rising high into the sky. As it cools down, it reaches a point called the dew point, where the moisture condenses into tiny water droplets or ice crystals. When these droplets or crystals grow heavy enough, they fall…
If you are looking up at the sky on a bright afternoon—you see puffy cotton-like shapes drifting lazily, sometimes turning into dark, ominous masses before a storm. These are clouds, nature’s way of storing and transporting water across the globe. But how exactly do these fascinating formations come into existence? Let’s explore in detail: What…
