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Summary

Environment Class 14

## BRIEF OVERVIEW OF PREVIOUS CLASS (1:09 PM)

## CLIMATE CHANGE AND GLOBAL WARMING (1:13 PM)

- **Climate:**
- The **climate** refers to the atmospheric conditions of a place for a long period measured by a minimum of 30 years.
- **UNFCCC** defines climate change as a change of climate attributed directly or indirectly to human activities that alter the composition of the global atmosphere and which is in addition to natural climate variability observed over a comparable period.

## CAUSES OF CLIMATE CHANGE (1:23 PM)

- **Milankovitch cycles** result in changes in insolation, seasonal variations, etc.
- Volcanic eruption
- Thermodynamic circulation
- Continental drift
- **Anthropogenic Factor:**
- Deforestation
- Change in land use pattern
- Urbanization
- Agriculture and Animal Husbandry
- Energy intensive activity
- **Radiative forcing:**
- The changes that have a cooling effect are called negative forcing. **For example**, an increase in Aerosol concentration causes a higher reflection of sunlight and cooling of the surface.
- A variety of physical and chemical changes which can affect the global energy balance and force changes in the earth's climate are called radiative forcing.

## GLOBAL WARMING (2:10 PM)

- **Green Houses Gases:**
- The major GHGs arranged in increasing order as per the global warming potential***: C02***
- ***Global Warming Potential:***
- *![GWP](https://i.ibb.co/ygc7RvD/GWP.png)*
- ***Global Warming Potential** is the measure of how much energy the emission from one tonne of gas is observed over a given period relative to the emission of 1 tonne of CO2.*
- ***CO2:***
- ***Sources:** fossil fuel, agriculture, industries (thermal, cement, etc), deforestation, etc*
- ***Note:** For the keeling curve kindly refer to the PPTs shown by the faculty.*
- ***Methane:***
- ***Sources:**Wetland, ruminant emissions, biomass burning, termite emissions, landfills, geological sources, wild animals, etc.*
- ***Nitrous oxides:***
- ***Sources:** Agricultural soil management, wastewater treatment, stationary combustion, chemical production, transportation, and manure management etc.*
- ***Note:** Kindly refer to the PPTs shown by the faculty for a better understanding of fluorinated gas.*

*## EVIDENCE OF CLIMATE CHANGE (2:58 PM)*

- *1. **Global rise in the temperature:** AR6 of IPCC has observed that the average temperature of the earth has increased by 1.09°C since the late 19th century, out of which 1.07°C is due to human factors.*
- *2. **Ocean warming:** The top 100 m of oceans have shown warming of more than 0.33°C since 1969.*
- *3. The **hottest year on record** is 2023. Every decade has been the warmest compared to its previous.*
- *4. **Global sea level rise** of 20 cm on average in the last century.*
- *5. **Melting of snow cover:** The Arctic sea Ice has decreased by 40% in summers and 10% in March. It is expected that within 15 years there will not be any ice left in the Arctic region during the summers*
- *6. **Retreat of glaciers** in almost every mountain i.e. Himalayas, Alps, Rockies and Andes, etc.*
- *7. **Ocean acidification:** Since the beginning of the Industrial Revolution the acidity of the oceanic surface has increased by 30%.*

*## IMPACT OF CLIMATE CHANGE (3:15 PM)*

- *Increased **melting of glaciers** will impact the flow of river water.*
- *More **glacial lakes** are formed which may result in **GLOF**.*
- *It reduces the availability of water in the long run, creating **water stress**.*
- *Impact water supply to **agriculture***
- *Crops may become more **water-intensive***
- *Increase rate of evaporation and disturbance in the condensation process due to an increase in air temperature.*
- *Intensity and frequency of rainfall changes.*
- *Increases the **occurrences of drought** due to irregular rainfall.*

*## OCEAN WARMING (3:20 PM)*

- ***Ocean warming** causes more heating of the sea surface and disturbs various atmospheric phenomena such as the formation of cyclones, and the occurrence of El Nino, La-Lina and Indian Ocean dipole.*
- *The warming results in the formation of more stable and stratified upper layers.*
- *It leads to less mixing of deeper and colder nutrient-rich water with the surface.*
- *The oxygen supply to the lower layer is limited creating oxygen-minimum zones.*
- ****At higher temperatures, dissolved oxygen in the water decreases.****
- *The high temperature of the water is harmful to marine species. **For example:** Coral bleaching.*
- *Higher temperature increases metabolic activities causing an increase in the oxygen demand.*

*## OCEAN ACIDIFICATION (3:30 PM)*

- ***Ocean acidification** is increasing the acidity level of ocean water due to the observation of higher levels of CO2 is called ocean acidification.*
- *It reduces the availability of carbonate ions in the water and increases the bicarbonate ions.*
- ***Note:** For Impact kindly refer to the handout shared by the faculty.*

*## OZONE DEPLETION (3:44 PM)*

- ***Ozone** is an allotrope of oxygen with three oxygen atoms.*
- *It is a pale blue gas with a **pungent odour**.*
- *It is mainly present in the stratosphere (90%) and helps in the filtration of UV rays.*
- *When UV rays pass through the ozone layer 100% of UV-A, 90% of UV-B and 5% of UV-C rays are absorbed.*
- ***UV B** - skin burning, Skin Cancer, etc.*
- ***UV A** - maximum tanning*
- ***UV C** - skin cancer, DNA damage, etc (most dangerous).*
- ***Ozone Oxygen cell:***
- ****O2 (Oxygen) + UV rays = O3 (Ozone)****
- ***O3 + Uv rays= O2***
- ***Ozone-depleting substance (ODS):***
- ***Chlorine:***
- ***Substances:** CFC, Carbon tetrachloride and Methyl Chloroform*
- ***Sources:** Refrigerant, propellants of aerosol, fire extinguisher, etc*
- ***Bromine:***
- ***Substances:** HBFC, Methyl Bromide*
- ***Sources:** Fire extinguishers and pesticides*
- ***Nitric Oxide:***
- ***Substances:** Nitrous oxide*
- ***Sources:** Industrial and agricultural use*
- ***Why they were used?***
- *Most of these compounds were non-corrosive, non-inflammable, low toxic chemically stable, and long lifetime.*

*## THE TOPICS FOR THE NEXT CLASS: CONSERVATION*