Chinese Radar Base in Sri Lanka to Keep an Eye on India: Report

The radar at Dondra Bay could track movement of Indian Navy vessels travelling to Andaman and Nicobar Islands. There are also apprehensions that it can monitor the Kudankulam and Kalpakkam Nuclear Power Plants, along with refuelling activities in these facilities.

New Delhi: China is considering setting up a radar base in the jungles near Dondra Bay of Sri Lanka which will be able to monitor India’s strategic assets in south India, the activities of the Indian Navy in the Indian Ocean Region and US military activities in Diego Garcia, reports the Economic Times.

The radar could also keep an eye on the Kudankulam and Kalpakkam nuclear power plants.

Dondra Bay is located at the southern-most tip of Sri Lanka and is historically significant, as it was once the capital of the island nation.

The newspaper states that the Aerospace Information Research of the Chinese Academy of Sciences could be involved in this project which will be detrimental to India’s strategic interests across the region. The radar could track movement of Indian Navy vessels travelling to Andaman and Nicobar Islands. There are also apprehensions that radar can monitor Kudankulam and Kalpakkam Nuclear Power Plants and refuelling in these facilities, reports the newspaper.

India has been concerned about Chinese activities in Sri Lanka. Last year Chinese surveillance vessel Yuan Wang 5 docked at the Hambantota Port after the Sri Lankan government conceded to the Chinese request despite Indian warnings. Sri Lanka allowed the vessel to dock at Hambantota and remain for six days for refuelling and logistics supplies.

Unable to repay its debt, Sri Lanka gave China a controlling equity stake and a 99-year lease for Hambantota port, which it handed over in December 2017.

The Uncertainty and Obsolescence Vikram Sarabhai Saw in India’s Future

“I believe that the present is particularly threatening to those like you who embark on a professional career for the first time,” Sarabhai said in a talk to the students of IIT Madras in 1965.

Today marks the birth centenary of Vikram Sarabhai, the celebrated industrialist and innovator popularly considered to be the father of the Indian space programme.

Sarabhai founded the Physical Research Laboratory in Ahmedabad in 1947. Three years later, the Government of India set up the Department of Atomic Energy (DAE) under the aegis of Homi J. Bhabha. The two organisations subsequently undertook research on atmospheric and space science and spaceflight as well as supported similar efforts around the country. In 1962, Sarabhai set up the Indian National Committee for Space Research (INCOSPAR) with Bhabha’s support. INCOSPAR assumed responsibility for space-related studies and activities that the DAE had until then overseen. Seven years later, it was supplanted by a larger institution called the Indian Space Research Organisation, marking the start of India’s formalised spaceflight programme.

Apart from shaping ISRO in its formative years, he also established the Indian Institute of Management, a community science centre and, with his wife Mrinalini, the Darpana Academy of Performing Arts, all in Ahmedabad. Sarabhai was famously committed to pressing the applications of science and technology to the needs of the nation, and contributed to national efforts in nuclear power generation, industrial organisation, market research and physical science research as well. He passed away on December 30, 1971.

By way of commemoration, the text of Sarabhai’s convocation address delivered at IIT Madras on August 1, 1965, is presented in full below.

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Things have changed a great deal during the last five years. Jawaharlal Nehru, Kennedy and Khrushchev are gone from the international scene. Nations already armed to the teeth have continued to engage in a spiralling arm s race and bombs rain every day from the skies over North and South Vietnam. Violence is rampant the world over. There is disenchantment with aid and with military alliances. Manned exploration of the moon and, in this country, the pursuit of engineering studies do not have the same glamour as before. Political life in Red China, in the United States and in India is chaotic and social goals perceived with cynicism. What is happening around us? Has the uncertain world come to stay with us?

The affliction is not peculiar to us; rich nations and poor ones, large and small, powerful and weak, those in military alliances, the nonaligned and the neutral, all manifest the same symptoms. The scenario is different, in France, in the United States, in Poland, in Japan and in India. And so are the methods by which societies try to deal with these problems. But a common thread runs through all these. I wish today to share with you some of my thinking, for, I believe that the present is particularly threatening to those like you who embark on a professional career for the first time.

Everyone here is undoubtedly familiar with the expression ‘three raised to the power of eighteen’. It is a large number: 38,74,20,489, thirty-eight crore, seventy-four lakh, twenty thousand, four hundred and eighty-nine. What it means in dynamic terms is quite dramatic. If a person spreads gossip to just three others and the same is passed on by each of them to three others, and so on in succession, in just eighteen steps almost the entire population of India would share the spicy story. Note that if each step takes one hour, 90% of the people hear the gossip for the first time only during the seventeenth and the eighteenth hours. Indeed, during the whole of the first 80% of the time, the process affects merely 11% of the population. Even though each individual is partaking in the chain reaction exactly like all the others, who preceded him, that is, he receives information from one person and passes it on to three others, the social impact at a late stage of development hits like an avalanche.

Villa Sarabhai in Ahmedabad, 1951-1955

Villa Sarabhai in Ahmedabad, 1951-1955

When we have a new infection, initially it is barely perceptible, but as a biological organism multiplies through successive generations, at a certain moment it suddenly permeates through the whole system. You can observe this fascinating phenomenon in making dahi or yoghurt, or thayir as you call it here. In the same way, information, knowledge, innovation, people and things diverge rapidly and their collective effects appear suddenly even though the basic process in each case has proceeded over a long time span.

When considering the social implications of technological change, one usually mentions the effects of the machine age on society through automation and imposed conformity. But these are trivial compared to the wider social implications of innovative man, who with curiosity, ingenuity and ambition, tries to reach out from his natural environment, and starts divergent processes. In nature, left to itself, control is maintained through an ecological balance. Order is not imposed from above, but arises through the interaction of each unit with its environment in a dynamic equilibrium. On the other hand, inherent in a programme of accelerated development, there is a suppression of some of the natural constraints which prevent divergence. And as the rate of innovation, of discovery and of everything else in the world gets faster and faster, so does the obsolescence of people and things become ever more acute. In contrast, biological development continues at its own pace. The child still requires nine months to develop in the womb. His life cycle of learning, of adolescence, as a house-holder and as an elder, who lays down the law, remains essentially unchanged.

Also read: A Wreath of White Roses Over the Ruins of Mehrangir, Homi Bhabha’s Home

The situation is aggravated because of the increase in the life span of the human being. The contradiction between desired longevity and a world of increasing change is obvious. An inevitable result of all this is the disillusionment of the young concerning the understanding and behaviour of the middle aged and the old. Equally serious is the inability of those who wield power and influence over world affairs to adopt values and behaviour, inherent in an order where accelerating change, rather than stability, is dominant. I suggest that today we witness a crisis of obsolescence.

An undated photograph of Vikram and Mrinalini Sarabhai with their son Karthikeya. Credit: Mid-Day

The qualitative change which has occurred in the last decade with the development of atomic energy, with the exploration and use of space, with the advent of electronics and computer sciences, is a manifestation of the divergent human function which has suddenly overtaken the world. What we have witnessed so far, dramatic as it is, is probably pedestrian compared to what we can expect in the future.

We have heard of the feasibility of areas of Earth’s surface illuminated during the night with sunlight through giant reflectors attached to satellites. We have also heard of weather modification, by increasing precipitation of rain in certain regions through artificially seeding clouds. There has been a suggestion of putting into orbit a belt of dust particles over the equator such that it would change the distribution of solar energy penetrating to different regions of the earth. It is claimed that such a belt could reduce the heat in the tropics and scatter more to high latitudes, providing a temperate climate even in the polar regions. This has many frightening possibilities because the level of the oceans would rise and submerge many inhabited areas.

New leads in biology and genetics pursued relentlessly are creating situations with implications few have thought through. Population control using the pill has tied up into knots theologists, wishing to interpret the sayings of the holy books in terms of current needs of society and new concepts of life. Just as doctors are faced with the problem of determining what death is before spare parts surgery would be justified, international lawyers rack their brains to determine an objective criterion for identifying where air space ends and outer space begins in which national sovereignty does not exist.

Affairs in the 1960s are largely in the hands of those who were already grown up when the Second World War broke out. Their learning experience and their theoretical knowledge relates principally to a period when the world was qualitatively different. The concepts of national sovereignty, of international spheres of influence, and power politics of the classical type have hardly changed even though we are constantly watched from satellites in outer space above us, and our security is threatened not merely by hostile neighbours, but by the actions and indiscretions of distant powers. What is the relevance of foreign bases in the context of long range missiles and nuclear submarines lurking unseen and silent on ocean floors? Is the Indian Ocean Indian any longer? How shall we preserve democratic states where the media of mass communications provide means of instantly reaching downwards from centres of authority, but, short of public agitation, there is no authorised channel for the reverse feedback for controlling the political system between elections?

ISRO chief K. Sivan during an event to mark Vikram Sarabhai's birth centenary. Credit: PTI

ISRO chief K. Sivan during an event to mark Vikram Sarabhai’s birth centenary. Credit: PTI

What should be the goals of education in a world of obsolescence? We find ourselves largely unprepared to meet the new situation. In real life, it makes a lot of difference how we view these occurrences. We have the situation in India, in comm on with many other countries, of students challenging the authority of universities and of the establishment. Those who assume that the students are indisciplined and wayward suggest that getting them involved in some activity such as the NCC would set matters right. On the other hand, if one regards protests of students at Columbia, at the Sorbonne and at Banaras as manifestations of a deeper malaise of society, the powers that be would introspect rather than preach. There is no easy solution.

Also read: Are ISRO and India Willing to Do What It Takes to Make It in Space?

But there is, I believe, much that we can learn from an analogue that we find in the peaceful applications of atomic energy more precisely, in the technique of extracting energy liberated in the fission of uranium. As is well-known, when an atom of the [uranium-235 isotope] is hit by neutrons, it has a tendency to split into two lighter atoms, the combined weight of the splinters being less than the weight of the original atom. In the process of fission, not only is the difference of m ass liberated as energy, but additional neutrons are released. When these neutrons hit other fissile atoms, a chain reaction occurs and the process can continue like the divergent spread of gossip.

We require a critical mass of uranium before the chain can be self-sustaining and indeed, when there is no other control device, the mass explodes through the sudden liberation of a large amount of energy on reaching criticality. This is what constitutes an atom bomb based on fission. When we wish to extract useful power out of the self-sustaining chain reaction of fission, we have to prevent the divergent release of neutrons, and of energy in the mass of the system.

This needs the establishment of a large number of control loops which constantly and simultaneously sample the level of the reaction at various points of the reacting volume and sensitively adjust the position of neutron absorbers, strategically placed at various positions in the core of the reactor. Divergent trends are almost instantly compensated. An operator can shut down the reactor by pushing neutron absorbers into the core. But no reactor can be maintained in a steady state of self-sustained activity, necessary for providing useful energy, on the basis of exclusive reliance on gross controls operated with imperfect feedback loops. Indeed, the control of potentially divergent systems relies on sensitive information loops which operate quickly in response to minute changes of activity.

Vikram Sarabhai was featured on a commemorative stamp the Government of India issued in 1972. Credit: India Post

Vikram Sarabhai was featured on a commemorative stamp the Government of India issued in 1972. Credit: India Post

What can we learn from this analogue in the social context? That control of the divergent human function cannot be maintained through the macro system of a super government. We need a system which perm its an infinite number of micro control loops spread through the fabric of society. An authoritative regime can inhibit the divergent human function, but only at the cost of inhibiting development itself. Ironically, free societies are the ones which are most prone to the social impact of run away divergencies. It is in such free societies that the power of the super state, the super authority in education and for developmental tasks, is most difficult to sustain.

I am intrigued by how closely this line of thinking brings us to Vinaobaji’s and Jayaprakash’s ideas on social and political organisation. We are faced with the problem of the divergent human function manifesting itself on the world scene, while in India we are still trying to shake ourselves free from poverty. We have, I believe, to create a social system and a pattern of development which is based not on monolithic organisations operating impersonally at an all-India level or even at the level of the states but in units where the feedback loop has high fidelity communication and a quick response.

Also read: U.R. Rao, ISRO Chairman Who Helped India’s Space Programme Settle Down

I am convinced, for instance, that our education system would immeasurably benefit if it were liberated from the monopolistic privileges under which universities take hold of all educational matters at a certain level in allotted territories. There is no way in which a University Grants Commission or an affiliating university can ensure educational standards. In the ultimate analysis, it is only the teacher in the classroom that can do anything in the matter. He has to be provided the freedom to innovate in education in a changing world and, for this innovation, he has to receive the trust of those who back him up. I would suggest that the most effective development of education can take place only when the teacher, the student, his parents and the outside environment can interact with one another, in a series of feedback loops, free from regimentation and irrelevant theories and principles preached from the top.

U.R. Rao inaugurates a bust of Vikram Sarabhai at Antariksh Bhavan, the ISRO HQ, New Delhi, 2004. Credit: ISRO

U.R. Rao inaugurates a bust of Vikram Sarabhai at Antariksh Bhavan, the ISRO HQ, New Delhi, 2004. Credit: ISRO

Engineers look forward to play a meaningful role in society. We are nationally poised to formulate a new Five Year Plan for development. Economists in the past have been prone to equate investments in hard facilities as necessary for economic growth. This is often true, but in the present context, it is largely fallacious. Twenty years after independence, w e find ourselves with a broad infra-structure of plants and facilities in the engineering industries which are largely under-utilised. We also find a number of well-established laboratories, without clear-cut developmental tasks which are meaningful in terms of national priorities. What is needed now is a major investment in design and developmental effort directed at indigenous capability for carefully chosen tasks, which are important to us.

As an example, I might cite a good transportation system: providing an inexpensive scooter or a cheap car; a mass communication system which brings television to every village in a decade; inexpensive power through the countryside based on optimisation of grids, with a combination of hydroelectric, atomic and thermal units; a defence system based largely on hardware related to our own strategic needs rather than one which is reliant on what our friends overseas choose to sell us, gift to us or help produce under their know-how. We can identify subsystems under each of these major tasks and we can create design and development groups which can operate with a wide measure of autonomy. They will require trust to be able to innovate.

All this is not a pipe dream. I hope we have the good fortune of realising these programmes before divergent functions in our society blow asunder all that we cherish.

14 Years After a Monster Tsunami, What Do We Know of the Quake That Caused It?

Efforts to fully characterise the sequence of events on that fateful day have brought scientists closer to predicting such hazards well in advance.

Note: This article was first published on December 26, 2018 and is being republished on February 20, 2019.

The Indian Ocean tsunami 14 years ago, on the morning after Christmas, was massive by any contemporary standard. The M9.3 earthquake that caused it emanated from a point near the west coast of Sumatra. It moved the seafloor by 10-20 m vertically and displaced trillions of tonnes of undersea rock, rippling through the 1,000-km-long Andaman plate boundary. The tsunami created as a result slammed into the coasts of 11 countries, from east Africa to Thailand, killing over 200,000 people.

Notwithstanding the several minutes to several hours between the quake and the tsunami reaching the costs, coastal communities were caught completely by surprise. There were no tsunami warning systems in place. There wasn’t any social memory of previous tsunamis preserved in the community psyche either; that might have helped deal with such disastrous situations.

As yet another anniversary of the episode dawns, let’s take stock of what we have achieved in terms of understanding large earthquakes and tsunamis in the Indian Ocean.

The 2004 disaster was considered unprecedented at the time – in its magnitude as well as transoceanic reach. Except for some isolated voices, the international research community had failed to anticipate such power lurking along India’s eastern seaboard.

Also read: Indonesia Searches for Survivors After Volcano Triggers Tsunami, Kills 281

The region has since witnessed many technological advances. The authorities have deployed offshore and deep ocean tsunami-observation systems, becoming able to issue early tsunamis warnings. The Indian National Centre for Ocean Information Services, with inputs from the India Meteorological Department, now tracks realtime quake data from a seismic network in the region.

In the same vein, the last 14 years have also been scientifically productive. During the last decade, many studies have endeavoured to understand the 2004 quake’s physics. Geological, seismological and GPS-based geodetic studies have focused on earthquake source properties, crustal deformation, tsunami sources and potential, and long-term forecasts.

Now, we know that such mega-earthquakes-cum-tsunamis have impacted the Indian coast in the past. The last 2004-type even occurred in the 14th century, destroying flourishing medieval ports like Kaveripattinam in modern Tamil Nadu.

A town in Miyagi prefecture, Japan, devastated by the earthquake and the tsunami on March 11, 2011. Credit: US Navy

A town in Miyagi prefecture, Japan, devastated by the earthquake and the tsunami on March 11, 2011. Credit: US Navy

But for all the experience and knowledge gained from tsunamis of the past, we were still surprised by the 2011 quake-and-tsunami off the Japanese coast. And this disaster occurred in one of the best-prepared countries in the world. Beyond its widespread material consequences, it served to caution us against nurturing an unrealistic sense of scientific and technological expertise in the face of such chaotic phenomena.

Nature has always been a storehouse of surprises. For instance, the 2011 tsunami apparently challenged much of the conventional wisdom in earthquake/tsunami science. It flew in the face of the belief that faults of certain lengths could break at predictable intervals, in the form of earthquakes of similar magnitudes. These quakes are dubbed ‘characteristic’.

But the 2011 quake may have been ‘composite’, consisting of multiple sub-events, as seismologists are starting to find. It probably started as an ordinary event that became a runaway process, forcing the upper part of the fault zone to break and displace the seafloor vertically. This action then pushed a large volume of water inland.

In the last seven years, scientists may have elicited a similar sequence of events in the 2004 Indian Ocean earthquake. Aside from the strain build-up and energy build-up/dissipation cycles, the fault blocks’ frictional properties appear to have had a major role in birthing the quake and determining if the rupture grew into a mega-quake. But what happened in the northern part – i.e. Andaman side – is still a bit of a mystery.

A large rupture in the seafloor near Aceh, Sumatra, ripped northwest for almost two minutes. After a 100-second pause, it continued northward towards the Andaman islands but 25% slower, and stopped five minutes later. It’s likely that the subsequent vertical displacement of land was also smaller in that area.

Efforts to fully characterise this sequence of events have brought scientists closer to predicting such hazards well in advance.

Earthquakes nucleate – or begin – tens of kilometres below the surface. At such depths, we don’t clearly understand the properties of rocks and their complex interactions due to the pressure, temperature and movement of fluids. It is also not possible to observe nucleation processes at those depths.

An animated GIF showing the tsunami propagating out after the 2004 earthquake off Sumatra. Credit: Wikimedia Commons

An animated GIF showing the tsunami propagating out after the 2004 earthquake off Sumatra. Credit: Wikimedia Commons

However, these barriers haven’t prevented us from finding other ways to make long-term forecasts. For example, scientists have combined satellite-based measurements, numerical models of crustal deformation and fault-specific geological studies to make long-term forecasts in some regions.

The success of earthquake prediction ultimately depends on being able to isolate any precursory signals that can be captured (years or even hours) before a big quake occurs. Though we don’t know how to do it yet, we know it’s likely possible. Recent insights into the 2004 earthquake has allowed geologists to cautiously suggest that it could’ve been anticipated months in advance.

Advances in GPS measurements are to thank for this. They have developed into an accurate way to record subtle fault-related movements as well as the rapid motion that occurs during earthquakes. Although some similar measurements were made before the 2004 quake, the data was properly evaluated only in this decade.

A 2015 study measured the movement of Earth’s surface at Port Blair using a space-based GPS system. (Disclosure: The author was one of the scientists who conducted it.) It was found that the GPS monitoring site in Port Blair had started to slip down from its original height between 2003 and 2004, suggesting a slow downward movement before the seismic monster struck.

Another group of researchers had used tide-gauge data from Port Blair to show that the sea level around the island changed in the same period, lending credence to the GPS data. It is now acknowledged that Port Blair was first rising up and then began to subside months before the earthquake.

The pre-quake downward slip is estimated to have been equivalent to an M6.3 quake. The magnitude could’ve been higher towards the plate boundary, located 200 km west of Port Blair.

Also read: Seven Years On, Japanese Live Uneasily With Seawalls After Tsunami

We have been able to use these details to piece together what likely happened in the Andaman side of the rupture around 2004. The fault along Sumatra and North Andaman had accumulated as much stress as it could have and was ready to rupture. But instead of one big blowout, it may have initially failed in the Andaman part, de-stressing as a slow slip near Port Blair starting sometime in 2003.

On December 26, 2004, there was a sudden release of energy and the fault propagated from Sumatra to the Andaman side in the northwest. This part of the plate boundary, which had already been releasing its stress in the pre-earthquake slow slip, caught up with the faulting but released its pent-up energy in lower doses. This is borne out by the fact that tsunami waves recorded on the Andaman coast had a lower amplitude than those on the southern Nicobar Islands and Sumatra.

This picture further stresses the importance of paying more attention to satellite-based geodetic data – such as in the study that revealed a precursory deformation under Port Blair.

An aerial view of the central Makran range in Pakistan. Credit: CanonS2/Wikimedia Commons, CC BY-SA 2.0

An aerial view of the central Makran range in Pakistan. Credit: CanonS2/Wikimedia Commons, CC BY-SA 2.0

Moreover, keeping an eye on the Andaman and Nicobar part of the eastern seaboard alone won’t suffice. We also need to focus on other problem spots, like the Makran range along the Gulf of Oman and the Myanmar coast in the northern Indian Ocean. Both of them have the potential to produce large tsunamis. The Makran range, spread through Iran and Pakistan, in particular could direct a tsunami’s energy towards India’s western coast – which hosts a number of critical facilities like nuclear reactors.

After the Japanese experience in 2011, we should be thankful that the 2004 tsunami had only a partial at the Kalpakkam nuclear reactor in Tamil Nadu and didn’t induce a full-blown catastrophe. Next time disaster strikes, the lessons learned from our past should stand in good stead, although we shouldn’t assume we are fully prepared either. As the geological dictum goes, the past is the key to the future.

C.P. Rajendran is a professor at the Geodynamics Unit, Jawaharlal Nehru Centre for Advanced Scientific Research and the Indian Institute of Science, Bengaluru.