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










alluvial >red>>black>>terai >>

















               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.


Tropical Peat Soils Under Different Land Uses - Gambut Kita
Peat soil is a type of soil that's formed from partially decomposed organic matter that accumulates in waterlogged areasIt's rich in organic matter and has a spongy consistency. 
How is peat soil formed?
  • 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. 
Properties of peat soil 
  • 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.
Where is peat soil found? 
  • 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.
Importance of peat soil
Peatlands are important ecosystems that store carbon and freshwater. 
They also help to adapt to extreme conditions such as high water and low oxygen. 


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 Nitrogenn organic matter 
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 













Temperature Inversion 





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:

  1. Air Sinks in High-Pressure Zones → Subsiding air compresses.
  2. Adiabatic Heating → As air descends, pressure increases, causing it to warm.
  3. Temperature Inversion Forms → Warm air layer develops above cooler air.
  4. 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. 


===========================================================





thunder storm formation 






















'image.png' failed to upload.

NORMAL 
easterly trade winds -east to west 
consider at  peru coast (s .america) 
flows towards east i.e australia 
austalia more rain --- india will also get more 

BUT 

EL-NINA  (not good for india )2 to 7 yrs 

Winds flows WEST to EAST 
Warm water at peru ,, (LOW pressure )
so less rain in india 
Heavy rains & floods in Peru, Ecuador, and parts of the U.S. 🌊🌧️


RegionEffects
Australia & IndonesiaDroughts, wildfires 🔥
IndiaWeak monsoons, crop failure 🌾
South America (Peru, Ecuador)Heavy rainfall, floods 🌊
North AmericaWarmer winters, stronger storms ⛈️
===============================================

LANINA 
Winds from 
peru (HP) 
towards australia -india 
SO MORE RAINFALL IN INDIA
======================================================



la NINA - 


  • 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).









Comments

Popular posts from this blog

MY MAPS NOTES

Geography ,Landforms and their evolution (chapter 07 NCERT CLASS 11 SUMMARY )

Revolt of 1857 overview

ENVIRONMENT TABLES CHARTS , IMP KEYWORDS ,Diagrams

RESOURCES -natural , -GEO- ECONOMY RELATED iNFRA n DEVelopment

BUDGET 2025-26 NOTES

modern history imp. pointers , Tables

environment -species pics

SCience and Tech CA Images

Science and Technology