The Social Consequences of India’s Heat Waves Spell Doom for the Working Poor

Deaths due to heat waves in India are usually reported as class- and gender-neutral numbers, hiding the irony of global warming that those least responsible for it are affected the most by it.

This article was originally published on June 24, 2016, and has been republished in light of the recent heat waves in North India.

“The time has come,” the Walrus said,
“To talk of many things:
Of shoes, and ships, and sealing wax
Of cabbages and kings
And why the sea is boiling hot
And whether pigs have wings.”
– Lewis Carroll, The Walrus and the Carpenter, 1872

The seas aren’t exactly boiling hot, but we are trying our best. Over 90% of all the excess heat trapped by carbon dioxide, methane and other greenhouse gases since 1970 has gone into the oceans. This has happened largely because of the high capacity of water to absorb and retain heat.

The amount of overall heat energy trapped by greenhouse gases is jaw-dropping. Between 1971 and 2010, the IPCC’s latest Assessment Report tells us that Earth gained 274 million million billion joules. James Hansen, one of the world’s most renowned climate scientists, put these bewildering numbers a little more colourfully. The excess energy trapped since 2005, he said in a TED Talk a couple years ago, is “equivalent to exploding 400,000 Hiroshima atomic bombs per day, 365 days per year”. We’ve  trapped, since 1970, the energy equivalent of four Hiroshima bombs every second.

Given this enormous amount of excess heat being trapped in Earth’s climate systems, it’s hardly surprising that one obvious, and widely-accepted, manifestation of global warming has been an increase in the geographical area, frequency and duration of heat waves – such as we have been experiencing in many regions of India this year. Globally, there’s no one definition of a heat wave. In most towns in the US, for instance, the most common definition is temperatures touching 90º F (about 32º C) for a period of three consecutive days. In Denmark, a heat wave is declared if temperatures cross a pleasant 28º C across the half the country’s landmass for three days.

India’s thresholds are a little higher than Denmark’s. They vary given myriad geographies and ecosystems, but a heat wave is usually declared if the maximum temperature of a place rises about 4-6º C over its 1971-2000 average. A heat wave is also declared when any place touches 45º C irrespective of what its normal is, and 40º C if the monitoring station is in a coastal area, again irrespective of the norm (according to a paper by D.S. Pai, et al, published in Mausam, October 2013). A recent discussion in the journal Nature by P. Rohini, M Rajeevan and A.K. Srivastava, covering the half-century 1961-2013, reveals “a statistically significant increase in frequency, duration and maximum duration of heat waves over India”.

The Indian Meteorological Department also has a category called ‘severe heat wave’, which is declared when a place’s temperature soars 6-7º C over its normal. These have recently been observed globally. In a paper published in the Proceedings of the National Academy of Sciences in 2012, James Hansen and others showed that extreme spikes in temperature had spread massively over the world’s landmass. “Probably the most important change,” they wrote, “is the emergence of a new category of “extremely hot” summers … [These] practically did not exist in 1951-1980, but in the past several years these extreme anomalies have covered of the order of 10% of the [world’s] land area.” The paper by D.S. Pai and others also mentions a noticeable increase in severe heat waves in India, both in the number of days and the geographical area affected in the decade 2001-2010, as compared to the previous four decades.

Why are these occurring? Increased heat waves over India are partly caused by an increased warming of the Indian Ocean during the past half century, and a consequence of the incredible amount of heat energy oceans are absorbing. But ocean and climate systems are extremely complex. For instance, heat waves are also somewhat influenced by the El Niño oscillation, reversing ocean currents of the equatorial Pacific that influence weather systems the world over. In fact, more than one paper recently suggested that heat waves occur in many parts of India in the year following an El Niño year, such as in 2016 following the massive El Niño of last year and which is only now receding.

A question that comes to mind is: how is global warming, and so much heat being absorbed by the oceans, influencing the strength or frequency of El Niños? On this key question for India, the jury is still out. But the paper by P. Rohini, et al, states that “the consequences of these changes [in sea surface temperatures of the Indian Ocean and the tropical Pacific] include an increased frequency of extreme El Niños. With warming of the tropical Indian Ocean and increased frequency of extreme El Niño events, more frequent and long-lasting heat wave events are likely over the Indian sub-continent in [the] near future.”

Heat waves and the working poor

If one leaves aside the rarefied class of people that lives with air-conditioning 24/7, the social consequences of this on most others in India are grave and growing. If and how people cope with heat waves depends on their occupation and context. For instance, earlier this year, desilting work being done by rural wage-labourers as part of ‘Mission Kakatiya’ in Telangana came to a standstill. The Indian Express quoted one of the contractors as saying, “We lost 15-20 days due to the heat wave. We could not work and even the Irrigation Department told us to be careful.” In Orissa, the environmental journalist Richard Mahapatra has reported that schools, colleges and government offices shift their timings of work to opening early in the day and close by noon. This has significantly reduced the number of deaths from heat waves in Odisha (as reported by the magazine Down to Earth). In Delhi, schools that are due to close for summer holidays around May 15 invariably declare holidays early, to the joy of innumerable school kids.

Not all are so lucky. Urban areas are teeming with occupations that force people to work through the day in the most grim conditions, or outdoors. Industrial areas such as Wazirpur in North Delhi have innumerable tiny factories in which sheets of steel or tin are being flattened by first superheating them; the heat within these workplaces – where a working day of 12-14 hours with a half-hour break for lunch is commonplace – is intolerable on any Delhi summer’s day, let alone during a heat wave. Heat waves affect lakhs of other urban poor; those who work as security guards, an occupation whose numbers have exploded in most towns those selling stuff at street lights, and the homeless who have nowhere to hide. Construction workers, who are forced to do what is often back-breaking work through the heat, and often comprise women, form a high proportion of those killed in heat waves in some states. The profit-motive that drives capital along with the precarious nature of such work can literally take a deadly toll.

Deaths due to heat waves in India have been in the thousands – in the years 1998, 2002, 2003 and 2015 in particular. Numbers, which are how the deaths are usually reported, are class- and gender-neutral. It’s one of the grave ironies of global warming that those least responsible for it are affected the most by it. What’s more, the numbers are very likely underestimates. Heat stress affects different organs, whose failure may be understood and recorded as the immediate cause of death, when it is recorded at all. Say, heart failure among the elderly or malnourished, but the underlying cause is heat stress that the body has been unable to cope with. And underlying that is global warming, which plays itself out in complex ways. The tricky causal connections between global warming and death due to a heart attack of an infirm agricultural worker in interior Telangana we may never be able to tease out.

There’s another growing effect of heat waves whose causal connections with global warming may be tricky to establish in India. A recent landmark study linked a rise in chronic kidney disease (CKD) worldwide and global warming. “Epidemics of CKD consistent with heat stress nephropathy, are now occurring across the world,” it said. Richard Johnson, one of its lead authors, said, “A new kind of kidney disease, occurring throughout the world in hot areas, is linked with temperature and climate and may be one of the first epidemics due to global warming.” This has obvious and huge implications for India, given high background/‘normal’ summer temperatures, water stress and unequal access to water, increasing humidity, rising heat waves and spreading droughts.

Finally, we tend to forget or perhaps don’t appreciate that all human beings have an absolute physiological limit to cope with a combination of heat and humidity. That threshold is 35º C of wet-bulb temperature (wbt). In contrast with regular temperature, a layman’s way of thinking about or measuring wbt is by putting a wet cloth over the bulb end of a thermometer and allowing normal air to play over it. Our bodies generate heat due to metabolic processes even while at rest, which we usually shed by sweating or conduction. More than six hours in conditions over 35º C of wbt and our body loses its capacity to shed heat. Certain death from hyperthermia ensues, even in the shade and even for those supremely fit. Novak Djokovic would expire if he spent over six hours in these conditions doing nothing.

Most places in the world are still some distance from 35º C wbt; the highest currently is about 31º C wbt. But a paper published late last year reveals (paywall) that places in the Middle East – Dubai, Abu Dhabi and Doha among them – a region where lakhs of Indian migrants live and work, will exceed 35º C wbt later this century if the world does not move away from a business-as-usual carbon emissions scenario now. What will its consequences be in hot and humid places in India, where millions work outdoors in non-air-conditioned spaces? For the elderly, the ill, children or those malnourished, the fatal threshold is lower. As average temperatures rise, what is currently an extreme heat outlier becomes increasingly frequent and commonplace. But we are talking of something even more dire: large tracts of land in India where millions now live becoming inhabitable; going, for some periods in the year, beyond the coping capacity of human physiology.

That’s an added reason to tackle global warming with urgency, in addition to the many that are already known. If the world is unable to quickly, and sharply, lower its current emissions trajectory, it’s not the oysters in the Lewis Carroll poem but our proverbial goose that will be cooked.

Nagraj Adve is a member of the India Climate Justice collective. He works and writes on issues related to global warming.

Climate Agreements Aren’t Going to Stop What Southeast Asian Cities Have Coming

“Even if we manage to keep warming to the limits agreed in Paris, the impacts on human health from heat stress are likely to increase substantially as global temperatures climb.”

“Even if we manage to keep warming to the limits agreed in Paris, the impacts on human health from heat stress are likely to increase substantially as global temperatures climb.”

Credit: vimalmehra/pixabay

Credit: vimalmehra/pixabay

Bengaluru: Sweltering under the blazing sun, sweat streaking down my forehead, I ran into the cool interiors of a taxi, vowing never to step out during the day until the rains came. It was barely summer, but the headlines of the discarded newspaper already warned of an impending heatwave. I looked up from the newspaper for a moment to see construction workers outside labor on, probably unaware of the heat warnings.

If you think summers are getting worse each year, you’re not alone. Those studying the climate for a living are thinking the same thing. This steady warming stresses humans more. Projections have suggested that in some regions the heat may even exceed human tolerance levels by the end of the century, with such episodes of dangerously high heat becoming more frequent than they are now. There have been efforts globally to limit warming, but simply meeting these targets may not be enough for large cities, especially in Southeast Asia.

As far back as 1896, the Swedish chemist Svante Arrhenius deduced a relationship between temperature and global carbon dioxide levels. Carbon dioxide and water vapour maintain Earth at an average of 15° C because they absorb the Sun’s heat and act as a natural greenhouse. Arrhenius suggested that, if carbon dioxide levels doubled, Earth would become warmer by 5° C.

Since then, there have been numerous studies warning of a warming earth and its serious consequences. Because of this growing concern, the United Nations adopted a framework for climate change mitigation in 1992 that all UN member states have ratified. This paved the way for the negotiation of various global climate change treaties such as the Kyoto Protocol adopted in 1997, and the more recent Paris Agreement in 2015. The main aim of the Paris Agreement is to limit the rise in global average temperature to less than 2 °C above pre-industrial levels, and pursue efforts to limit it to less than 1.5 °C above pre-industrial levels.

The heat index

But that may not be enough for the highly populous Southeast Asian cities, claims a new study led by Tom Matthews of the Liverpool John Moores University, Liverpool. “Our study shows that even if we manage to keep warming to the limits agreed in Paris, the impacts on human health from heat stress are likely to increase substantially as global temperatures climb,” said Matthews.

Matthews and his team used both temperature and humidity in their projections, a measure called the heat index, which is a better measure of how we feel than simply using the temperature. For example, it is generally much more difficult to tolerate the stickiness of Chennai than the dry heat of New Delhi, implying that the heat index of Chennai is higher than that of New Delhi. This is because it is much harder to cool down by evaporation of sweat when it is very humid, making the heat stress on humans much greater.

And at higher temperatures, the heat index increases significantly more than the corresponding increase in temperature. “We were suspicious that the warming permitted by the Paris targets could therefore result in large increases in heat stress,” said Matthews, explaining why they undertook the study. They looked at the temperature increases permitted by the Paris Agreement, and higher values, taking into account a scenario where the agreed limit could not be met, and projected the global heat stress burden.

The heat stress burden for a 1.5 °C rise in temperature is projected to be 5.7-times that experienced during 1979-2005, rising to about 12-times if there is a 2 °C warming. If we fail to limit warming to the targets agreed and there is a 4 °C rise, this burden may reach fully 75-times that of the reference period.

What this means is that heatwaves, like the deadly one in 2015 over northern India and Pakistan will not be a one-off event, but will occur every year, and possibly be more intense.

Mapping the projected heat stress values to the world’s most populous cities, the study estimated an additional 350 million people could face the burden of heat stress by the end of the century compared to the 1979-2005 period. Indian cities such as New Delhi, Kolkata, Chennai and Ahmedabad that already experience large heat stresses will experience consistently larger increases. Of the top 10 cities that are projected to have the highest heat stress burden, six are in India, Pakistan and Bangladesh. Ho Chi Minh city, Vietnam, is projected to have one of the largest increases in heat stress burden because of a combination of dramatic population increase and sharp increases in the heat index.

Of the increases permitted by the Paris Agreement, we have already used up 0.8 °C between 1986 and 2015. That only allows 1.9- (1.5 °C) and 3.4- (2 °C) times the warming already experienced, which are ambitious targets. This in turn translates to a significantly greater increase in the heat stress because of its non-linear relation with temperature.  

Under a dire scenario when the planet warms by 4 °C, places such as New York City and Bangalore can become heat-stressed, developing heat-index values similar to Ahmedabad and Hanoi, respectively.

Heat action plans

Krishna AchutaRao, a climate scientist at IIT Delhi, said, “As expected, especially in the tropics, big cities, the megacities, are all going to get a) more populated, and b) they are going to get hotter and more humid. Therefore there are going to be more people exposed to the kind of deadly heat [waves] that we’ve experienced in the recent past in India.” He also added that the had study assessed hazards and exposure but hadn’t assessed vulnerability. “Not everybody who is exposed to this heat is going to be equally affected by it” Somebody out on the street selling their wares – or construction workers labouring in the heat, the old, very-young or sick – will evidently be more vulnerable than somebody working in an office building.

This is something Matthews is interested in working on in the future. “I see much potential for working on heat stress adaptation–helping vulnerable communities live with more frequent episodes of extreme heat,” said Matthews. Apart from limiting the earth from getting any warmer, there are a range of adaption methods that can be implemented, like making cities greener or painting urban roofs white. “While promising, these design solutions principally reduce excess urban heat. They can’t eliminate the danger of extreme heat driven by large-scale high temperature and humidity events.”

He added, “Beyond engineering solutions, improved preparedness – of individuals to city authorities to emergency response teams – can help reduce the impacts of extreme heat.”

One such action in India is the Ahmedabad Heat Action Plan. It strives to make people, hospitals and emergency response teams aware of extreme heat and ways to tackle it. It was first drafted in 2013 by the Ahmedabad Municipal Corporation with the help of national and international academic experts, and is said to have reduced heat-related deaths by up to 25%.

Other cities, like Nagpur and Bhubaneswar, are also interested in developing such a plan, according to AchutaRao. Although the India Meteorological Department issues heat-wave warnings and long-term forecasts, the Ministry of Earth Sciences has also been urging states and cities to develop their own heat actions plans, he added.

Although the study is only an indication of what we may be in for in the future, the increase in the frequency and intensity of heatwaves over the Indian subcontinent in the last few years, along with their occurrence earlier in the year, serves as a warning. We can no longer afford to deny the important role of mitigation and helping societies adapt to an intensely warming world.

Lakshmi Supriya is a freelance science writer based in Bangalore.

Rising Heat Could Cut 3.6% of India’s Daylight Work Hours

Excessive heat while working, creates occupational health risks and reduces work capacity and labour productivity.

Excessive heat while working, creates occupational health risks and reduces work capacity and labour productivity.

Credit: Reuters

Credit: Reuters

India is set to lose 3.6% of annual daylight work hours by 2025 due to rising temperatures, reveals an IndiaSpend analysis of data in a new UN report.

The loss of daylight work hours could increase to 5.2% in 2055 and 8% in 2085, assuming a consistent rise of 2.7°C, according to Climate Change and Labour: Impacts of heat in the workplace, released by the UN Development Program (UNDP).

Exploring the link between rising temperatures and productivity loss, the UNDP report said South Asian countries will be the most affected by rising temperatures; European and South American countries will be the least affected. The report is the latest to warn of productivity losses resulting from climate change.

The worst-affected countries globally will be Burkina Faso, Cambodia, Pakistan and Maldives.

In May, India recorded its highest-ever temperature of 51°C in the town of Phalodi in the western state of Rajasthan. In the southern state of Telangana, as many as 315 people died this year (until May) from heat-related causes, and as IndiaSpend reported in April 2016, heat-wave deaths in India increased 296%, or three times, over the last 23 years.

The year 2015 was the third-warmest year recorded in India in India since record-keeping began in 1901 and as many as 22,563 people have died in heat waves across India between 1992 to 2015, as reported.

Notes: 1. The percentages refer to potential annual daylight hours when workers slow down or take more rest due to the rising heat, leading to health and productivity issues. 2. These are preliminary and indicative results for a selection of countries based on model data in an IPCC analysis. An updated analysis is due in 2016. The data is based on a working intensity of 300 watts, which is a reasonable mid-point level for a variety of jobs in agriculture, industry and construction. The share work capacity (work losses at very intense physical work) would be twice as high as the numbers in the table. Share work indicates a job that cannot be done by one worker, such as building a road or a bridge.

Source: Climate Change and Labour: Impacts of heat in the workplace.

Excessive heat while working, generally at temperatures above 35°C, creates occupational health risks and reduces work capacity and labour productivity. Maintaining a core body temperature close to 37°C is essential for health and human performance, and large amount of sweating as a result of high heat exposure while working creates dehydration risks.

Outdoor workers with a moderate and heavy workload exceeded the threshold limit value of 28°C and experienced 18-35% productivity loss, according to this 2014 study from Chennai.

4°C  temperature rise can lead to 13.6% work-hour loss

The projected annual loss of daylight work hours in 2085 can further rise if temperatures do.

In India, an 8% loss in daylight work hours can be reduced to 7%, if the temperature rise is limited to 2.4°C, but the work-hour loss will surge to 13.6% if the temperature rises by 4°C.

A large part of southern India, the eastern and western coasts, which have been unaffected by heat waves, are projected to be affected after 2070 and will be exposed to extreme heat-stress conditions, intensification of heat wave and heat-stress leading to increased mortality, IndiaSpend had earlier reported.

Source: Climate Change and Labour: Impacts of heat in the workplace

Source: Climate Change and Labour: Impacts of heat in the workplace

India will lose 1.8% of its GDP due to climate change

Those in the lowest-income group – heavy labour and low-skill agricultural and manufacturing jobs – are among the most susceptible to climate change, according to the UNDP report.

India has 263 million farm workers and 13 million workers in factories. Without changes to current global behaviour on climate change, India would see economic losses equivalent to 1.8% of annual GDP by 2050, widening to 8.7% by 2100, predicted this 2014 report from the Asian Development Bank (ADB).

If mitigation and adaptation steps keep the temperature rise below 2°C, economic losses could be limited to below 2% of GDP by 2100, the ADB report said.

Labour productivity impacts could reduce output in affected sectors by more than 20% during the second half of the century, according to estimates in the Intergovernmental Panel on Climate Change (IPCC) 5th assessment report. The global economic cost of reduced productivity may be more than $2 trillion by 2030.

Devanik Saha is an independent journalist based in Delhi.

This article originally appeared on IndiaSpend.org, a data-driven, public-interest journalism non-profit. Read the original article.