18 March 2016, ECOS, Building disaster resilience systematically. The cost of replacing essential infrastructure damaged by disasters in the next 35 years is estimated to reach $17bn according to the latest set of reports from the Australian Business Roundtable for Disaster Resilience and Safer Communities. The reports, Building Resilient Infrastructure and the Economic Costs of Social Impact of Disasters, outline the costs associated with replacing essential infrastructure damaged by disasters and provide an overview of the direct costs of physical damage with the total economic cost of disasters. In 2015, the total economic costs of disasters exceeded $9bn, a figure that is projected to double by 2030 and reach $33bn per year by 2050 – funds that could be apportioned elsewhere on other major national projects. And as Heinrich Eder, CEO of reinsurer Munich Re, noted, these projections are based only on economic and population growth; they do not even include the increasingly detectable effects of climate change. These are big, and socially traumatic, numbers. Long-term they have the same sort of potential to create holes in national and state budgets as our ageing population does—the subject of repeated Intergenerational Reports and eventual decisions about adjusting retirement age. It is clear to us, based on our work, that investing much more in disaster resilience as a nation will reduce physical damage, avoid social disruption and trauma, and lessen this capricious burden on state and national budgets. In fact, estimates suggest that well-targeted investments in resilience could result in significant savings for the government. Read More here
Yearly Archives: 2016
14 March 2016, The Guardian, Severe coral bleaching worsens in most pristine parts of Great Barrier Reef. Expert blames global warming, as coral bleaches when water temperatures go above a certain threshold for an extended period of time. Damage to parts of the Great Barrier Reef has worsened, leading authorities to raise the alert to the second-highest level, indicating severe local coral bleaching. The bleaching is worst in the most pristine and remote parts of the reef north of Cairns, according to Terry Hughes, convenor of the National Coral Taskforce. “It’s the jewel in the crown of the Great Barrier Reef and it’s now getting a quite a serious impact from this bleaching event,” he said. “The northern reefs are bleaching quite badly now.” Hughes said it appeared there was some coral death occurring in northern reefs. Russell Reichelt, the chairman of the Great Barrier Reef Marine Park Authority said the area around Lizard Island, 250km north of Cairns, and sites further north, had fared the worst. The US National Oceanographic and Atmospheric Administration predicts bleaching conditions to worsen over the coming weeks. The world is currently in the grips of the third global coral bleaching event. Coral bleaches when water temperatures are raised above a certain threshold for an extended period of time. Hughes, director of the ARC centre of excellence for coral reef studies at James Cook University, said although the strong El Niño occurring now is partly to blame for the bleaching event, the real culprit is global warming caused by carbon emissions. Read More here
14 March 2016, The Guardian, February breaks global temperature records by ‘shocking’ amount Warnings of climate emergency after surface temperatures 1.35C warmer than average temperature for the month. February smashed a century of global temperature records by “stunning” margin, according to data released by NASA. The unprecedented leap led scientists, usually wary of highlighting a single month’s temperature, to label the new record a “shocker” and warn of a “climate emergency”. The NASA data shows the average global surface temperature in February was 1.35C warmer than the average temperature for the month between 1951-1980, a far bigger margin than ever seen before. The previous record, set just one month earlier in January, was 1.15C above the long-term average for that month. “Nasa dropped a bombshell of a climate report,” said Jeff Masters and Bob Henson, who analysed the data on the Weather Underground website. “February dispensed with the one-month-old record by a full 0.21C – an extraordinary margin to beat a monthly world temperature record by.” “This result is a true shocker, and yet another reminder of the incessant long-term rise in global temperature resulting from human-produced greenhouse gases,” said Masters and Henson. “We are now hurtling at a frightening pace toward the globally agreed maximum of 2C warming over pre-industrial levels.” Read More here
14 March 2016, The Conversation, Tipping point: how we predict when Antarctica’s melting ice sheets will flood the seas. Antarctica is already feeling the heat of climate change, with rapid melting and retreat of glaciers over recent decades. Ice mass loss from Antarctica and Greenland contributes about 20% to the current rate of global sea level rise. This ice loss is projected to increase over the coming century. A recent article on The Conversation raised the concept of “climate tipping points”: thresholds in the climate system that, once breached, lead to substantial and irreversible change. Such a climate tipping point may occur as a result of the increasingly rapid decline of the Antarctic ice sheets, leading to a rapid rise in sea levels. But what is this threshold? And when will we reach it? What does the tipping point look like? The Antarctic ice sheet is a large mass of ice, up to 4 km thick in some places, and is grounded on bedrock. Ice generally flows from the interior of the continent towards the margins, speeding up as it goes. Where the ice sheet meets the ocean, large sections of connected ice – ice shelves – begin to float. These eventually melt from the base or calve off as icebergs. The whole sheet is replenished by accumulating snowfall. Floating ice shelves act like a cork in a wine bottle, slowing down the ice sheet as it flows towards the oceans. If ice shelves are removed from the system, the ice sheet will rapidly accelerate towards the ocean, bringing about further ice mass loss. A tipping point occurs if too much of the ice shelf is lost. In some glaciers, this may spark irreversible retreat. Read More here