I begin with a proposition. There are a great many pressing problems in the world. There is population growth and economic development, with attending pressures on resources - including food and that other essential, water. There is a continuing global security crisis, augmented by the rise in terrorism. There is the chronically inequitable distribution in resources between the rich nations of the North and the poor nations of the South. And there is the steadily growing body of evidence for a major reorganization of the global climate regime.

My proposition is that the last of these is the most serious threat - not only because it will profoundly affect the lives of our children and our grandchildren in a direct way, but also because it will interact powerfully with every single one of the other problems I have listed.

Let me begin with the science underlying climate change. Last week I helped organize a symposium and briefing session on climate science for press, policy-makers, and the public, supported by the Hewlett Foundation and with co-sponsorship from the Conference Board. We had ten of the most distinguished climate scientists in the United States, led off by Sherry Rowland, the Nobel Laureate in Chemistry. The purpose was to make a careful assessment of the science - what we know for sure, what we think likely, and what are interesting but unproven possibilities.

So here is a short summary of what we know. General Circulation Models - climate models that take into account variations in the sun's energy, volcanic activity, and other natural phenomena - explained fluctuations in average global temperature very well over most of the past thousand years. But for the past hundred years, these same models faithfully reproduce global temperature history ONLY if they include the greenhouse gases - carbon dioxide, methane, and chlorofluorocarbons - that are by-products of human economic activity. That is why the average temperature of the globe has risen by about one degree F, and the sea level has risen by between 10 and 20 cm., in the last century. The primary causative agent is carbon dioxide, which in preindustrial times was about 280 ppm/v and has now reached 380ppm/v. It is rising continually as the activities that produce it are proceeding on a business as usual basis. That is because the failure of the Kyoto protocol - a failure both because its targets were inadequate, and also because they were unattainable by many of the participating nations - has left us without any basis for meeting the goals of the 1992 Framework Convention on Climate Change. Just to remind us, the US is a signatory and a party to that agreement, under which we are committed to limit atmospheric concentrations of greenhouse gases to avoid "dangerous anthropogenic interference with the climate system."

Why, a dozen years later, is there some doubt about the dangers of this interference? The C02 we add to the atmosphere will stay there; its average residence time is a century. There is no disagreement about whether average global temperature will rise; it will. The scientific debate is about how much. For the future we depend again on the General Circulation Models. It's reassuring that when applied to past climates in "back-casting" efforts, like the example I gave a moment ago, these actually predict climate history so accurately. Perhaps more interesting, they regularly somewhat underestimate the magnitude of the real climate changes - that is, Nature regularly turns out to be harsher than the models suggest. Projecting the models into the future, the Intergovernmental Panel on Climate Change, and an evaluation by the National Academies prepared at President Bush's request, estimate that by the end of this century, the increase in average global temperature will be between 1.4 and 5.8 degrees Centigrade.

Why such a range? These models, like most, contain some uncertainties. Some of these are scientific: how increased cloud cover might affect the outcome, since clouds can either cool the climate by reflecting sunlight from above, or warm it by trapping heat that is leaving from below; how changes in the earth's albedo due to melting ice might accelerate heating, and so on. Aerosols produced by volcanic eruptions have a cooling effect, as the eruption of Mt. Pinatubo did in giving us two unusually cool years in the early 90's. Other uncertainties are economic and social: we don't know how national policies and international agreements will serve to restrain the amount of greenhouse gases we are adding.

These uncertainties - about half due to the models themselves, and the rest to social and economic unknowns -- have provided arguments for those who prefer to postpone economically difficult approaches for controlling greenhouse gas emissions. But it is important that even at the very lowest estimates, there will be substantial changes in the nature of human life on the only planet we currently occupy. The rather modest impacts of the past century have already produced profound changes in regional climate dynamics. Substantial ice-sheet melting and retreat is taking place both in the Arctic and in the West Antarctic ice sheet. In the Arctic, where climate warming has been extreme, sea ice is sharply diminished and rivers become ice-free much earlier. Low latitude mountain glaciers are shrinking; the famous snow-capped summit of Kilimanjaro will be bare within fifteen years, converting hundreds of old African safari shots into historic treasures.

Biological cycles are experiencing the effects of warming, with upward extensions of the range of Alpine flora and advances in the time of flowering or breeding by an average of 5 days per decade. The models have all also predicted more frequent and severe weather events, and we have had heat waves in the upper Midwest and Paris, accelerated beach erosion on coasts all over the world, and disastrous floods and landslides in Central America.

That is now, but of course we are more interested in the future. What the models tell us unambiguously is that the climate system is headed for further disruption. The standard scenario foresees a steady, ramp-like increase in average global temperature, with a concomitant rise in sea level, but records of past climate tell us that it is riddled with abrupt changes - something that the models fail to predict well. A possible alternative involves a change in major ocean circulation patterns - especially in the North Atlantic, where a clockwise gyre brings warm equatorial water up via the Gulf Stream. As it flows Northward and then crosses Eastward, it is cooled by the atmosphere, becomes more saline through evaporation, and then sinks to return as a cold deep current. If large discharges of fresh meltwater or rain made this water less dense, it could fail to sink and thus disrupt the entire cycle.

A fictionalized version of such a scenario appears in the disaster film "The Day After Tomorrow," which you should see only for amusement. Beyond that silliness lies a real prospect that a gradual change in average global temperature could intercept the threshold for some non-linear, dynamic process, triggering abrupt changes in either direction. Of course there is uncertainty: we are engaged in a large-scale, uncontrolled experiment on the only planet we have.

Let's consider some collateral impacts. A group of us at Stanford was asked by the Carnegie Commission on Preventing Deadly Conflict to look - among other things -- at ways in which environmental change might alter the circumstances under which human populations might be placed. Climate change was an important variable. One example we looked at was the impact of sea level rise, along with storm surges from extreme weather events, on the Ganges-Brahmaputra delta. Flood disasters already occur there regularly. 15 million people live within 2 meter above sea level, and are vulnerable to abrupt displacement. We know they will have to go somewhere; in the past they have fled in much smaller numbers to Bengal. The security problems arising from a massive influx of a traditionally hostile population, combined with an almost certain high level of cholera infection, are not difficult to imagine.

Water is a desperately important resource in most parts of the world, and drought is often followed by famine or emigration. Here in the US, warmer winters threaten mountain snowpacks and will soon demand the revision of interstate and international water allocation agreements. Maritime rivers are already undertaking management steps to deal with saline intrusions due to sea level rise or storm surges. In Great Britain, the barrier that protects London from occasional flooding of the Thames estuary is now being used six times a year compared to less than once a year in the 1980's.

Agriculture, of course, is the most essential of human activities. The regional distribution of global warming impacts may be at least temporarily kind to temperate-zone food production. But the models all predict an increased incidence of mid-continent droughts as climate change progresses, and we know that the American Midwest has in the past experienced droughts both deeper and longer than the one in the 30's that led to the Dust Bowl migrations. Irrigation is an answer to drought, but in the six High Plains states, dryland wheat production depends upon the Ogallala Aquifer, a buried ice-age storage well that is being so rapidly depleted that it is already unusable in its southern portion. And in the tropics, where people are poorest and capacity to adapt is minimal, the consequences of even modest warming will be far more serious.

Infectious diseases are spread by vectors, like the Anopheles malaria mosquito, that have their own patterns of reproduction, movement, and climate sensitivity. In parts of Africa where vertical topography dominates, warmer and rainier seasons cause malaria incidence to rise in higher-altitude locations. In a warmer and wetter world, more of the same can be expected.

So climate change is not an isolated problem. Instead, it is likely to interact with most of the other problems humans face all over the world. Thus I hope that this meeting will help encourage us to prepare a sound portfolio of risk-reducing measures. These will not, I must tell you, bring us out of the woods. Our destiny is partly built in -- to the heat that is already locked into our oceans, to the greenhouse gases that are already in our atmosphere and will increase by another 50% or more no matter what we do, and to the justified economic appetites of the developing world. What we will be talking about, it should be clear, are ways of limiting the damage to manageable levels, NOT preserving the status quo. We lost that years ago.

So the contemporary policy challenge amounts to a bet about risk: are the consequences of business as usual likely to entail costs greater than those of beginning to mitigate those consequences now? Other nations - the UK, several EU countries, and Japan - are making substantial commitments. Some industries - British Petroleum, Royal Dutch Shell, and Swiss Re, for example - have undertaken steps of their own. The insurance burden from the exploding rates of coastal erosion and storm damage has pushed the insurance industry to lead. If companies fail to participate in emissions reduction and join with others to resist such measures, questions are already being raised. If you believe so strongly that climate change is a myth, Swiss Re might say, then surely you won't mind a climate-related events exclusion from your Directors and Officers insurance policy.

But we can't count on voluntary actions, and the United States so far has only announced a long-range research program that, although it looks reasonable, makes NO current commitments to mitigate our contribution, about a quarter of the world's, to the global warming problem. We must have a more aggressive national policy to purchase insurance against this risk.

It will not be cheap. We have old, coal-fired power plants in this country; it may take subsidies to replace them with modern, less carbon-intensive facilities that run on natural gas. States like mine are already driving the transportation sector to ultra-low emission, and that may move the domestic industry in a positive direction. Some of us will have to give up our reflex opposition to nuclear power and begin comparing its risks realistically against those of global climate change. Although the room for alternative energy sources (photovoltaic, wind, geothermal) is limited, these options need encouragement. Energy conservation measures have, at several times in the past, turned economic predictions on their head by their success, and the right incentives could yield real benefits there.

The portfolio I have just described is needed, but will not be enough. We know that market-based mechanisms for emissions control can work, because they did in the 1990 Clean Air Act Amendments that limited SO2 emissions. The bill proposed by Senators McCain and Lieberman would mandate a cap-and-trade program for controlling carbon dioxide emissions. Similar systems are being considered by regional assemblages of states in the Northwest and the Northeast, and that may encourage the development of a national system - which could then build trading relationships with other nations that are moving toward similar regimes. A case for this approach is elegantly made in the Council on Foreign Relations Policy Initiative on Climate Change, by my colleague David Victor.

The United States is in a position of natural leadership here. It is the most powerful nation - and the world's leading producer of greenhouse gases. Plainly it is in its own national interest, in multiple ways, to reduce its consumption of fossil fuels. To see it failing in this most vital, globally sensitive matter is a national embarrassment.

The audio version of this television program may be downloaded via the link below, using Realplayer. Click on the link for March 31, 2004.

Political science professor and APARC director emeritus Daniel I. Okimoto has received the Japanese Foreign Minister's Commendation. This commendation is awarded is in commemoration of the 150th anniversary of the U.S.-Japan relationship. The years 2003 and 2004 mark the 150th anniversary, respectively, of American naval officer Commodore Perry's leadership of a squadron of sailing sloops and steam-powered warships into Edo Bay (now Tokyo Bay) in 1853; and the signing of the Treaty of Peach and Amity in 1854.

The commendation is awarded to 158 individuals and organizations in Japan and the United States who have contributed to enhancing the U.S.-Japan relationship. Okimoto received the award based on his research on Japan's political economy, foreign policy, the U.S.-Japan relationship, and increasing the understanding of Japan in the United States. He has hosted a series of exchanges among legislators from the United States and Japan to build understanding between the two countries. Okimoto has also written about the Japanese American experience in his autobiography, American In Disguise.

In a May 14 lecture hosted by the Center on Democracy, Development and the Rule of Law, Francis Fukuyama, PhD -- professor of international political economy at Johns Hopkins University and renowned author of The End of History and the Last Man -- discussed the problem of weak, underdeveloped nation-states; the effectiveness of various approaches to strengthening such states; and the importance of culture, context and history in the task of state-building. His lecture, titled "State-building: A Framework for Thinking about the Transfer of Institutions to Developing Countries," drew a full room of attendees to the Bechtel Conference Center in Encina Hall

A former member of the RAND Corp. and the U.S. Department of State who has written widely on issues of democratization and international political economy, Fukuyama first presented a framework with which nation-states can be evaluated according to two key criteria: the strength of the state, and the scope of its functions. The first refers to a state's ability to enforce its own laws and policies; the second refers to how involved the state becomes in carrying out various societal functions, ranging from basic functions such as maintaining law and order and protecting public health, to more "activist" functions such as running industries and redistributing wealth.

Fukuyama asserted that from a development standpoint, nation-states should be strong but should carry out only the minimum necessary functions. He said that only one country he has studied -- New Zealand -- has effectively moved toward this ideal in recent years. He noted that many struggling, developing nations, such as Brazil, Mexico, Pakistan and Turkey, are overly ambitious in their scope -- attempting to run vast industries, for example -- but are weak and unable to carry out their policies because of factors like corruption. Other states that Fukuyama identified as "failed states," such as Haiti and Sierra Leone, are both limited in scope and weak, attempting to carry out only the most basic governmental functions and not doing it very well.

Fukuyama then discussed and evaluated various approaches to strengthening developing nations. He noted that in recent years much emphasis has been placed on encouraging such nations to reduce the scope of their functions, through deregulation and privatization, but said the effectiveness of this approach is now in question. A more effective approach, he said, is helping weak nation-states build their own strong institutions, such as political parties, public health networks and central banking.

Unfortunately, Fukuyama said, sometimes the efforts of outside organizations to strengthen a country's institutions only make things worse, because solutions are imposed from outside rather than developed from within. "Ideally, we would want a country's own public health system to handle that country's problems with AIDS or malaria," he said. "But when you flood the country with your organization's own doctors and nurses and infrastructure, what do the local doctors do? They quit their government posts to get on the payroll of your NGO." In a few months or years, when the organization withdraws its support, Fukuyama noted, the system collapses, because it was not built to be self-sustaining.

At the end of his talk, Fukuyama emphasized the importance of understanding local culture, context and history in the task of state building. For example, he said, those who run programs aiming to reduce the spread of HIV/AIDS in Africa should consider working with traditional faith healers, as they are an important part of the healthcare system in Africa.

Beijing tries to read mixed U.S. signals in Korea diplomacy By John W. Lewis

For the past year China has led the quest for a negotiated solution to the Korean nuclear crisis. It facilitated and hosted three-way talks with the United States and North Korea a year ago this week and two sessions of the six-party talks (adding South Korea, Japan and Russia) in August and February. Its officials crisscrossed the globe to explore potential areas of common interest and compromise and this week hosted North Korean leader Kim Jong Il to explore options for the beleaguered Korean Peninsula. Yet, in each of the formal talks, the Chinese have been discouraged by the minimal results. They are now questioning U.S. intentions toward Korea and, in the longer term, toward China.

Beijing considers the unchecked expansion of North Korea's nuclear weapons to be a real possibility, and its reasoning starts with the record of U.S. policies toward nuclear proliferation. That record, the Chinese argue, is mixed and often contradictory. As a result, China worries that Washington might continue to tolerate the program so long as Pyongyang did not cross key red lines, such as the transfer of nuclear materials to terrorists.

Whatever Beijing's past position on nuclear matters, many senior Chinese now regard nuclear weapons on their border to be a direct threat to their national security and suspect Washington of downplaying that danger. For them, it is no great leap to the conclusion that the unfettered growth of the Korean program might embolden others in Asia, including Taiwan, to acquire nuclear weapons despite verbal opposition from Washington. Beijing's leaders can easily imagine how that nightmarish turn of events would undermine the nation's drive toward modernization and end strategic cooperation with the United States.

Despite the fact that all parties at the six-party meeting in February endorsed the dismantling of the North's nuclear weapons program, the Chinese fear that the talks may be dead in the water. Following that meeting, they began to debate other ways to resolve the crisis. They had already reorganized the leadership team responsible for North Korean affairs, and that team had begun acting to prevent the worst case, including offering further inducements to Kim Jong Il this week. Whereas last fall the talk of deepening U.S.-China cooperation on Korea pervaded the news, now, especially after Vice President Dick Cheney's uncompromising stand on Korea and Taiwan last week, the reverse is occurring.

What China can do in these circumstances is quite limited. Its influence on North Korea is largely determined by what the United States does or doesn't do. By refusing to negotiate on a staged process leading to the eventual dismantlement of Pyongyang's nuclear weapons, Washington has tacitly allowed the North's program to proceed. It has rejected proposals for a temporary freeze, technical talks and any interim steps short of the unconditional and complete ending of the program. The result is virtual paralysis.

Beijing has been able to work with North Korea only when it could find areas of potential compromise between Washington and Pyongyang. It cannot or will not act

alone to exert pressure because this would jeopardize its influence on the North. Contrary to a widely circulated story, Beijing did not cut off energy shipments to North Korea for three days in 2003. Beijing would not take such a counterproductive action when its main influence with the North lies in the kind of quiet diplomacy being practiced this week with Kim Jong Il.

Many in Beijing are beginning to question whether there might be a more promising approach with Pyongyang. Should the Chinese, South Koreans and Russians conclude that making progress toward the common goal of the North's complete nuclear disarmament is out of reach, for example, they reluctantly might translate their joint offer of aid in February into a quid pro quo for a partial agreement, such as a limited freeze, that would allow the situation to stabilize. China could worry that such an independent action could endanger the common front with Washington. At the same time, it could calculate that the United States would be sufficiently pleased with any solution that halted the North Korean nuclear program.

None of these developments may come to pass, of course, but who could have imagined a year ago that Washington would have permitted the situation to deteriorate to the present point?