geography Phenomena pictures
MHWs are defined as prolonged periods of unusually high sea surface temperatures. Specifically, they occur when seawater temperatures exceed the
90th percentile for at least five consecutive days
SOIL PROFILE
Saline soil+gypsum= fertile 😃- Alluvial soils of the northern plains —> transported soils —>, therefore, lack humus —> lack nitrogen [That is why we need to use nitrogenous fertilisers in the northern plains!].
- Exception: the Ganga-Brahmaputra delta region is rich in humus.
- Peat soil forms over thousands of years in wetlands like swamps, marshes, and bogs.
- It's formed from the remains of plants like sphagnum moss, herbs, shrubs, and small trees.
- The organic matter decomposes very slowly due to a lack of oxygen.
- Peat soil has a high organic content, usually above 75%.
- It has a dark brown to black color.
- It has a low bulk density and high total porosity.
- It can swell and shrink when it gets wet and dries.
- Peat soil is found in all regions, but it's more common in the temperate and cold zones of the Northern Hemisphere.
- Peatlands cover more than half of the world's wetlands.
Here is a comprehensive table on different types of soils in India, their characteristics, locations, associated flora and fauna, and the key chemicals they are derived from:
Soil Type | Characteristics | Locations | Plants & Crops | Chemicals | |
---|---|---|---|---|---|
Alluvial Soil 🏞️ | - Fertile, rich in minerals 🌱 - Loamy & clayey texture - Retains moisture well 💧 | Indo-Gangetic Plains (Punjab, UP, Bihar, West Bengal), Coastal regions | Rice, Wheat, Sugarcane, Cotton 🌾 | Silica, Potash, Lime (caco3) phosphoroc rich |
|
Black Soil (Regur-REGADI) 🖤 | - Clayey, moisture-retentive 💧 - Rich in humus & nutrients - Swells when wet, cracks when dry | Maharashtra, Gujarat, MP, Karnataka, Telangana | Cotton, Jowar, Millets, Pulses 🏵️ | Iron, Magnesium, Lime,Alumina lack in |
|
Red Soil ❤️ | - Reddish due to Iron Oxides 🔴 - Porous, not very fertile - Deficient in lime & humus | Tamil Nadu, Odisha, Chhattisgarh, Andhra Pradesh | Groundnut, Ragi, Potato, Tobacco 🥔 | Iron Oxide, Potash, Aluminum))) 😭N , P -POOR |
|
Laterite Soil 🌋(brick making) | - Highly leached due to rain ☔ - Rich in Iron & Aluminum - Poor in organic matter | Western Ghats, Kerala, Karnataka, Assam, Meghalaya | Tea, Coffee, Cashew, Rubber ☕ | Iron, Aluminum, Silica | |
Arid Soil (Desert Soil) 🏜️ | - Sandy, low humus, poor moisture retention - High salt content | Rajasthan, Gujarat, Haryana | Bajra, Barley, Date Palm 🌵 | Calcium Carbonate, Gypsum | |
Mountain Soil ⛰️ | - Found in hilly & forested areas - Rich in humus, acidic in nature | Himalayan regions (J&K, Himachal, Arunachal) | Apples, Tea, Spices, Maize 🍏 | Iron, Potassium, Humus | |
Peaty & Marshy Soil 🌊 | - Rich in organic matter & humus - Waterlogged & highly acidic | Kerala, West Bengal, Sundarbans, North-East India | Rice, Jute, Coconut, Spices 🌾 | Organic Carbon, Nitrogen, Sulfur | |
Saline USARA& Alkaline Soil ⚡ | - High salt content, infertile - Found in dry, arid areas | Gujarat, Rajasthan, UP, Haryana, Punjab | Barley, Mustard, Cotton 🌿 | salts like Sodium, Potassium, Magnesium |
Would you like any modifications or additional details? 😊
💩REH ,THUR ,CHOPAN -LOCAL SALINE SOILS
This occurs most often on clear nights when the ground cools off rapidly by radiation. If the temperature of surface air drops below its dew point, fog may result.
This kind of temperature inversion is very common in higher latitudes. In the lower and middle latitudes, this kind of inversion gets destroyed easily during the daytime.
Formation Process:
- Air Sinks in High-Pressure Zones → Subsiding air compresses.
- Adiabatic Heating → As air descends, pressure increases, causing it to warm.
- Temperature Inversion Forms → Warm air layer develops above cooler air.
- Stable Atmosphere → Prevents vertical mixing, trapping pollutants.
common in areas located under large high-pressure centres.
Such conditions occur in the northern continents in winter and
over the subtropical oceans.
This temperature inversion is also called upper surface temperature inversion because it takes place in the upper parts of the atmosphere.
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thunder storm formation
Region | Effects |
---|---|
Australia & Indonesia | Droughts, wildfires 🔥 |
India | Weak monsoons, crop failure 🌾 |
South America (Peru, Ecuador) | Heavy rainfall, floods 🌊 |
North America | Warmer winters, stronger storms ⛈️ |
- El Niño: A warming of the ocean surface,or above-average sea surface temperatures (SST), in the central and eastern tropical Pacific Ocean.
- Over Indonesia, rainfall reduced
- while rainfall increases over the central and eastern tropical Pacific Ocean.
- The low-level surface winds, which normally blow from east to west along the equator (“easterly winds”), instead weaken or, in some cases, start blowing the other direction (from west to east or “westerly winds”).
- In general, the warmer the ocean temperature anomalies, the stronger the El Niño (and vice-versa).
- La Niña: A cooling of the ocean surface, or below-average sea surface temperatures (SST), in the central and eastern tropical Pacific Ocean. Over Indonesia, rainfall tends to increase while rainfall decreases over the central and eastern tropical Pacific Ocean. The normal easterly winds along the equator become even stronger. In general, the cooler the ocean temperature anomalies, the stronger the La Niña (and vice-versa).
- Neutral: Neither El Niño or La Niña. Often tropical Pacific SSTs are generally close to average. However, there are some instances when the ocean can look like it is in an El Niño or La Niña state, but the atmosphere is not playing along (or vice versa).
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