Why is it in the news?
1. The India Meteorological Department has forecast above normal temperatures in most parts of the country this summer between April to June, including extended heatwave episodes that may last 10-11 days in central and eastern India, affecting Odisha, Jharkhand, Eastern UP in particular.
2. The Director General of IMD said that above normal heatwave days are likely in Rajasthan, Gujarat, Haryana, Punjab, Madhya Pradesh, Maharashtra, Uttar Pradesh, Bihar, Jharkhand, West Bengal, Odisha, Chhattisgarh,Telangana, Andhra Pradesh and Northern Parts of Karnataka.
3. Heatwaves over these regions can last for 4-7 days but it is expected that these can prolong to 10-11 days over Odisha, Jharkhand, Eastern UP in this summer season.
4. Heatwaves extending up to a week could be experienced during April over eastern India mainly over Odisha.
5. It is to be noted that heatwaves are common in the month of April over eastern India regions covering Jharkhand, Gangetic West Bengal, Vidarbha in Maharashtra and Gujarat and heatwaves continue for 1-3 days. But, this year it is expected that chances of extended heat waves will be in the month of April over the above regions.
6. Thus, except West Peninsular India, some parts of East Central and East India, North eastern regions and J & K, major parts of India would be in the grip of heatwaves in the summer season between the months of April to June.
What is the definition of heatwave and severe heatwave in India?
1. When the maximum temperature exceeds at a particular place between 4.5°C to 6.4°C above the normal temperature for two consecutive days. Or when the maximum temperature reaches at least 40°C in plains, 37° C in coastal areas and 30°C in hilly regions for two consecutive days, it is called a heatwave.
2. When the maximum temperature is increased to 6.5° C or more above the normal temperature of that region. Or if the maximum temperature exceeds 47°C in the plains, which persists for two consecutive days, it is called a severe heatwave.
3. For example, If the normal maximum temperature in Delhi for the month of April is 37°C, if the temperature on two consecutive days is recorded 42°C, it would qualify as a heatwave. If the temperature increases to 44°C which persists for two consecutive days, it would be classified as a severe heatwave.
Similarly, suppose the average annual temperature of Shimla, a hilly station, is recorded 27° C. If temperature increases 32° C, it would be called a heatwave. But, if the temperature goes to 34° C in Shimla for two days, it would be called severe heatwave.
4. Heatwaves are more common in the northern, central and eastern parts of India. The most affected states from heat waves in India are Rajasthan, Uttar Pradesh, Madhya Pradesh, Haryana, Punjab, Odisha, Jharkhand, Chhattisgarh, West Bengal, Telangana, Vidarbha in Maharashtra, Eastern Gujarat and Andhra Pradesh.
Increasing trends of heatwaves in India
1. It has been found that instances of heatwaves in the central, north west and south east region of the country had been growing at the rate of about 3 heatwave days per decade since 2000.
2.The year 2024 saw a total of 554 heatwave days across the country , that is, a sum of heatwave days in all states.
Thus, except Nagaland, Manipur, Mizoram and Tripura, almost the entire country experienced heatwaves.
3. It has also been found that there was a steady rise in the long duration heatwaves, sometimes going for 15 days at a stretch. The prolongation of heatwaves has a significant adverse impact on ecosystems, agriculture and public health.
What are the causes for the heatwaves and severe heatwaves in India?
Heatwaves in India are caused by the interaction between atmospheric high pressure systems, geographical features, climate change and human activities.
1. Meteorological factor
Northern India is situated in the subtropical high pressure belt of 30° N of latitude. In the summer season the high pressure belt shifts further northward, covering northern and western India.
Air rises near the equator due to intense heating , moves poleward at high altitude and becomes cold. The cold air descends around 30°N and S latitude due to the coriolis effect. The sinking air from high altitudes suppresses cloud formation, resulting in clear skies and continued solar heating. The hot air near the ground is trapped. Uninterrupted sunlight heats the ground continuously during the day, causing temperature to rise sharply. High pressure systems usually remain stationary or move slowly. This stagnation traps warm air over a region for extended periods leading to the prolongation of the heatwaves. The lack of strong winds prevents the dispersion of hot air, thereby, intensifying local temperature. In normal conditions warm air rises, forming clouds and rain on account of convection. But a high pressure system inhibits convection, thereby, reducing rainfall and moisture. This leads to dry, hot and stable atmospheric conditions typical of heatwaves.
Sometimes, high pressure systems get blocked by other weather patterns, causing them to persist for days, thereby, intensifying the heatwaves. The jet system naturally meanders due to temperature differences between polar and tropical air masses. Sometimes these waves amplify and become stationary, forming a blocking pattern. For example, in 2010, Russian heatwave was caused by blocking high pressure systems that remain stationary over western Russia leading to record breaking temperature and wildfires. Similarly, in India, the blocking system can delay monsoon onset, thereby, causing prolonged dry spells and heatwaves.
Sometimes a heat dome is formed, thereby trapping hot air under a high pressure system. The dome acts like a lid, preventing cooler air from mixing in thereby, causing prolongation of heatwave conditions. High pressure pushes the clouds away from the dome. Hot air expands upward into the atmosphere but high pressure pushes warm air down, thereby, causing air compression leading to heat waves.
Delayed or weak monsoon increases the duration of hot weather.
Weak western disturbances lead to reduced pre-monsoon showers, thereby, causing prolongation of heatwaves.
The local wind called loo originates from the Thar desert. It blows from west to east. It is a dry wind and heats up to more than 50° C.
Cities with concrete structure and limited vegetation trap more heat.
2.Climate change
Increased greenhouse gas emissions have raised global temperatures worldwide. Since India already has a high baseline temperature because of its tropical position, any further increase in temperature causes heat waves. In recent years, because of the climatic change and rising temperature, India is witnessing frequency of more heatwaves.
Loss of tree cover and consequent deforestation further aggravates heat waves.
High level of air pollution trap heat, thereby, exacerbating local temperatures.
3.Anthropogenic Activities
Industrial emissions, burning of crop residues and vehicle emission further increase temperature.
4.Atmospheric patterns
Warming of the Central Pacific Ocean and Indian ocean, thereby, causing El-Nino leads to hotter summers and weak monsoons in India. Weak monsoon causes prolongation of heatwaves in India.
Hot winds from Arabian peninsula and central Asia often increase temperature in northwestern India.
How does it impact India in the pre-monsoon period of summer season?
1.Heat waves may cause health issues like :
Exhaustion
Heat Stroke
Dehydration
Increasing risk of the vulnerable groups like the elderly, children, outdoor workers and people with pre-existing conditions.
Increased mortality
Heat related complications
lMental health issued like stress, irritability and fatigue
2.It can cause following impacts on agriculture
Decreasing productivity of different crops
Livestock stress, reducing the productivity of cattle and therefore low production of milk.
Increasing demand of water for irrigation
Severe impact upon Rabi crops
3.Heat Waves can cause
water scarcity
Food insecurity
Shortage of drinking water
4. Heat waves causes
Reduced income of farmers
Reduced labour productivity
Increasing use of air conditioning and cooling system leading to power shortage
Migration of rural poor to urban areas in search of livelihood
5. Heatwaves leads to
Wildfires
loss of biodiversity
urban heat islands thereby, increasing the temperature in cities.
How to mitigate the impact of heatwaves?
1.The impacts of heatwaves can be mitigated through following methods
Early warning system
Heat action plans that includes risk mapping, capacity, building and response protocols
Public awareness programme to educate public about heat related illness
Regular health check ups
Promotion of the use of heat resistance materials for clothing and shelters
People should be exhorted to stay indoors during peak hours between 11 AM to 4 PM.
Establishment of cooling centres
Medical preparedness
Mobile medical units
Urban greening
Cool roofs and walls
Ponds, lakes and fountains should be integrated in urban centres to moderate temperatures
Rescheduling of school, colleges.
Rain water harvesting to increase ground water recharge to ensure water availability during heatwaves
Efficient use of water through drip irrigation
Setting up of water distribution points in public places
Promoting heat resilient crops
Promoting agroforestry
Using organic mulch to maintain soil moisture and reduce surface temperature
Reducing carbon emission by promoting renewable energy and reducing fossil fuels to combat global warming.
Investing in research for heat resisting crops, advanced cooling technologies and sustainable urban planning.
Reducing urban heat islands by increasing greenbelts and reducing use of asphalt in cities.
Conclusion
Heatwaves are natural calamities. They cannot be prevented. But through multifaceted approaches like public awareness, healthcare preparedness, urban planning, water management and long term climate action, their impact can be mitigated and precious lives can be saved. Several assessments have shown that the implementation of heat action plan has not been adequate in India while the administration has been more interested to implement short term measure such as making provision for drinking water in public places, creating cool shades for workers or preparing hospitals for heat related diseases, the long term interventions like greening of the cities, rejuvenation of water bodies, creation of parks or open spaces are being ignored. The approach of different governments is reactive rather than proactive, they react to a heatwave event when it occurs. They do not do enough to deal with the problem in a more comprehensive manner. It should be understood that the impacts of heatwaves can be largely managed if timely actions are initiated.