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  • Trouble in the Antarctic David Spratt Climate Code Red

    08 Jun 2014
    Home  »  Uncategorized   »   Trouble in the Antarctic

    Trouble in the Antarctic

    Posted in Uncategorized By Neville On June 8, 2014

    Why this ad?
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    I am posting these items to allow readers access to scientific reports on what is
    happening in our polar regions. Scientists can only predict Ice Melt and sea level rise based on their studies. No one has a crystal ball that can give exact figures or indeed when events may happen
    Neville

    Typo correction

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    Neville Gillmore
    David Suggest would have to be be (omitted) Warming of 0.2°C from a month of …
    8:45 PM (2 hours ago)

    David Spratt
    many thanks, fixed.
    8:50 PM (2 hours ago)

    Neville Gillmore
    David.. Have you compiled a similar report on the Antarctic Icemelt please? I…
    9:08 PM (1 hour ago)

    David Spratt

    10:53 PM (3 minutes ago)

    to me
    Hi Neville,
    Sorry, i haven’t but I will when the Breakthrough conference is over in two weeks.
    Best single article was this piece by the lead researcher in the Guardian:
    Interesting what the research published in May found was very similar to the story we told in Climate Code Red in 2008 in Chapter 3:
    Trouble in the Antarctic
    Big changes are also underway at the other end of the world,
    in the Antarctic, where most of the world’s ice sits on the fi fthlargest
    continent. The majority of Antarctic ice is contained in
    the East Antarctic ice sheet — the biggest slab of ice on Earth,
    which has been in place for some 20 million years and which,
    if fully melted, would raise sea levels by more than 60 metres.
    Considered more vulnerable is the smaller West Antarctic
    ice sheet, which contains one-tenth of the total Antarctic ice
    volume. If it disintegrated, it would raise sea levels by around
    5 metres, a similar amount to what we would see with a total
    loss of the Greenland ice sheet.
    While it was generally anticipated that the West Antarctic
    sheet would be more stable than Greenland at a 1–2 degree
    rise, recent research demonstrates that the southern ice shelf
    reacts far more sensitively to warming temperatures than
    scientists had previously believed. Ice-core data from the
    Antarctic Geological Drilling joint project (being conducted
    by Germany, Italy, New Zealand, and the United States) shows
    that ‘massive melting’ must have occurred in the Antarctic
    three million years ago, during the Miocene–Pliocene period,
    when the average global temperature in the oceans increased
    by only 2–3 degrees above the present temperature. Geologist
    Lothar Viereck-Götte called the results ‘horrifying’, and
    suggested that ‘the ice caps are substantially more mobile and
    sensitive than we had assumed’.
    The heating effect caused by climate change is greatest
    at the poles, and the air over the West Antarctic peninsula
    has warmed nearly 6 degrees since 1950. At the same time,
    according to a report in the Washington Post on 22 October
    2007, a warming sea is melting the ice-cap edges, and beech
    trees and grass are taking root on the ice fringes.
    Another warning sign was the rapid collapse in March 2002
    of the 200-metre-thick Larsen B ice shelf, which had been stable
    for at least twelve thousand years, and which was the main
    outlet for glaciers draining from West Antarctica. An ice shelf
    is a fl oating sheet, or platform, of ice. Largely submerged, and
    up to a kilometre thick, the shelf abuts the land and is formed
    when glaciers or land-based ice fl ows into the sea. Generally,
    an ice shelf will lose volume by calving icebergs, but these are
    also subject to rapid disintegration events. Larsen B, weakened
    by water-fi lled cracks where its shelf attached to the Antarctic
    Peninsula, gave way in a matter of days, releasing fi ve hundred
    billion tonnes of ice into the ocean.
    Neil Glasser of Aberystwyth University and Ted Scambos
    from the NSIDC found that as glacier fl ow had begun to
    increase during the 1990s, the ice shelf had become stressed.
    The warming of deep Southern Ocean currents (which
    increasingly reach the Antarctic coastline) had also led to
    some thinning of the shelf, making it more prone to breaking
    apart. Scambos concludes that ‘the unusually warm summer
    of 2002, part of a multi-decade trend of warming [that is]
    clearly tied to climate change, was the fi nal straw’.
    Looking at the overall pace of events, Scambos says: ‘We
    thought the southern hemisphere climate is inherently more
    stable, [but] all of the time scales seem to be shortened now.
    These things can happen fairly quickly. A decade or two of
    warming is all you need to really change the mass balance …
    Things are on more of a hair trigger than we thought.’
    Much of the West Antarctic ice sheet sits on bedrock that
    is below sea level, buttressed on two sides by mountains, but
    held in place on the other two sides by the Ronne and Ross
    ice shelves; so, if the ice shelves that buttress the ice sheet
    disintegrate, sea water breeching the base of the ice sheet will
    hasten the rate of disintegration.
    In 1968, the Ohio State University glaciologist John Mercer
    warned, in the journal of the International Association of
    Scientifi c Hydrology, that the collapse of ice shelves along
    the Antarctic Peninsula could herald the loss of the ice sheet
    in West Antarctica. A decade later, in 1978, his views received
    a wider audience in Nature, where he wrote: ‘I contend that a
    major disaster — a rapid deglaciation of West Antarctica — may
    be in progress … within about 50 years.’ Mercer said that
    warming ‘above a critical level would remove all ice shelves, and
    consequently all ice grounded below sea level, resulting in the
    deglaciation of most of West Antarctica’. Such disintegration,
    once under way, would ‘probably be rapid, perhaps
    catastrophically so’, with most of the ice sheet lost in a century.
    Credited with coining the phrase ‘the greenhouse effect’ in the
    early 1960s, Mercer’s Antarctic prognosis was widely ignored
    and disparaged at the time, but this has changed.
    ( James Hansen says it was not clear at the time whether
    Mercer or his many critics were correct, but those who labelled
    Mercer an alarmist were considered more authoritative and
    better able to get funding. Hansen believes funding constraints
    can inhibit scientifi c criticisms of the status quo. As he wrote
    in New Scientist on 28 July 2007: ‘I believe there is pressure
    on scientists to be conservative.’ Hansen is responsible for
    coining the term ‘The John Mercer Effect’, meaning to play
    down your fi ndings for fear of losing access to funding or of
    being considered alarmist.)
    Another vulnerable place on the West Antarctic ice sheet
    is Pine Island Bay, where two large glaciers, Pine Island and
    Thwaites, drain about 40 per cent of the ice sheet into the sea.
    The glaciers are responding to rapid melting of their ice shelves
    and their rate of fl ow has doubled, whilst the rate of mass loss
    of ice from their catchment has now tripled. NASA glaciologist
    Eric Rignot has studied the Pine Island glacier, and his work
    has led climate writer Fred Pearce to conclude that ‘the glacier
    is primed for runaway destruction’. Pearce also notes the work
    of Terry Hughes of the University of Maine, who says that the
    collapse of the Pine Island and Thwaites glaciers — already the
    biggest causes of global sea-level rises — could destabilise the
    whole of the West Antarctic ice sheet. Pearce is also swayed by
    geologist Richard Alley, who says there is ‘a possibility that the
    West Antarctic ice sheet could collapse and raise sea levels by 6
    yards [5.5 metres]’, this century.
    Hansen and fellow NASA Goddard Institute for Space
    Studies researcher Makiko Sato agree:
    The gravest threat we foresee starts with surface melt
    on West Antarctica, and interaction among positive
    feedbacks leading to catastrophic ice loss. Warming in
    West Antarctica in recent decades has been limited by
    effects of stratospheric ozone depletion. However, climate
    projections fi nd surface warming in West Antarctica
    and warming of nearby ocean at depths that may attack
    buttressing ice shelves. Loss of ice shelves allows more
    rapid discharge from ice streams, in turn a lowering and
    warming of the ice sheet surface, and increased surface
    melt. Rising sea level helps unhinge the ice from pinning
    points … Attention has focused on Greenland, but the
    most recent gravity data indicate comparable mass loss
    from West Antarctica. We fi nd it implausible that BAU
    [‘business-as-usual’] scenarios, with climate forcing and
    global warming exceeding those of the Pliocene, would
    permit a West Antarctic ice sheet of present size to survive
    even for a century.
    Even in East Antarctica, where total ice loss would produce
    a sea-level rise of 60 metres, mass loss near the coast is greater
    than the mass increase inland (mass increase inland is caused
    by the extra snowfall generated from warming-induced
    increases in air humidity).
    While the inland of East Antarctica has cooled during
    the last 20 years, the coast has become warmer, with
    melting occurring 900 kilometres from the coast and in the
    Transantarctic Mountains, which rise up to an altitude of 2
    kilometres.
    Research published in January 2008 by Rignot and six of
    his colleagues shows that ice loss in Antarctica has increased
    by 75 per cent in the last ten years due to a speed-up in the
    fl ow of its glaciers, so that the ice loss there is now nearly as
    great as that observed in Greenland.
  • 700.000 homes at sea rise risk

    homes at sea rise risk

    700.000 homes at sea rise risk

    Posted in Climate chaos, Extreme weather and global warming By admin On May 30, 2009

    “Other scientists say the sea could rise metres in the next century. The director of the Fenner School of Environment and Society at

    the Australian national University, Professor Will Steffen, told the inquiry there was huge uncertainty among scientists about the rate

    of sea level rise and ‘the science … has progressed significantly since the publication of the IPCC (report) last year’. The observed

    rate of sea-level rise is tracking at or near the upper limits of the envelope of IPCC projections. With no further changes in the rate of

    sea level rise, this would suggest that sea levels in 2100 would be 0.75m to one metre above the 2000 levels. However, there was

    further uncertainty over the loss of polar ice sheets, particularly Greenland, which was melting rapidly. The concern is that a

    threshold may soon be passed beyond which we’ll be committed to losing most or all of the Greenland ice sheet. This would lead to

    6.0m of sea level rise (with enormous implications for Australia), although the time frame required to lose this amount of ice is

    highly uncertain, ranging from a century to a millennium or more.”

    “Insurance Australia Group actuary Tony Coleman said preliminary estimates of the value of property, homes, businesses and public

    infrastructure vulnerable to sea inundation ranged from $50 billion to $150 billion. The figure depends upon the extent of sea-level

    rise assumed and the effectiveness or otherwise of potential mitigation measures.”

     

    Professor Will Steffen, Australian National University Article : West Australian (Page 18), 17 Oct 2008

     

  • Climate Change Causes Volcanoes and Tsunamis

    Climate Change Causes Volcanoes and Tsunamis

    Iceland Volcano Could Power Up UK

    The UK government is planning power up Britain homes with the help of geo thermal energy.

    Bill McGuire, a professor of geophysical and climate hazards at the University College London, has discovered that climate change can lead to earthquakes, volcanoes and tsunamis.

    McGuire’s work, part of which can be read in “Waking the Giant: How a Changing Climate Triggers Earthquakes, Tsunamis and Volcanoes”, suggests that climate change is not only about floods and droughts. It can also lead to increased volcanic activity and increasing numbers of earthquakes.

    McGuire believes the Earth is very sensitive to change and even though the Earth’s crust seems to be safe, the rapid changes can result in its destabilisation.

    In 2010, Eyjafjallajokull – the ice-covered Icelandic volcano that spewed several million cubic meters of ash – brought European air traffic to a grinding halt. Last year, the tsunami that hit the eastern coast of Japan was the result of a cataclysmic earthquake.

    According to information in McGuire’s book, it is believed that the Earth underwent astonishing climatic transformations some 20,000 years ago. During this period, it transformed from a frigid wasteland of ice to the world we are more familiar with.

    The point is that during this dynamic episode, as the ice melted and sea levels subsequently rose, the pressure of the water acting on solid earth increased. The planet’s crust then bent and cracked, leading to resurgence in volcanic activity, a proliferation of seismic shocks and burgeoning giant landslides, according to an article McGuire wrote in The Guardian.

    McGuire concludes by saying that human activity seems to be increasing risks of a geologic backlash at the most inopportune time.

    He stresses that unless there is a dramatic and completely unexpected turnaround in the matter of handling resources and the planet, the long-term impact could be very “grim”.

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  • Scientists discover link between climate change and ocean currents during last six million years

    Scientists discover link between climate change and ocean currents during last six million years

    AJR_Resolution-F_BarrigaResearch vessel JOIDES Resolution arriving Lisbon after the expedition

    Scientists have discovered a relationship between climate change and ocean currents over the past six million years after analysing an area of the Atlantic near the Strait of Gibraltar, according to research published today in the journal Science.

    An expedition of scientists, jointly led by Dr Javier Hernandez-Molina, from the Department of Earth Sciences at Royal Holloway, examined core samples from the seabed off the coast of Spain and Portugal which provided proof of shifts of climate change over millions of years.

    The team also discovered new evidence of a deep-earth tectonic pulse in the region, as well as thick layers of sand within mountains of mud in a vast sheet, spreading out nearly 100km into the Atlantic from the Gibraltar gateway. The quantity of sand is far more than was expected and has been caused by the strength, speed and long duration of bottom currents flowing through the Strait of Gibraltar from the Mediterranean.

    “The sediments we examined show various shifts of climate change over millions of years”, Dr Hernandez-Molina said. “In addition, our findings could herald a significant shift in future targets for oil and gas exploration in deep-water settings. The thickness, extent and properties of these sands make them an ideal target in places where they are buried deep enough to allow for the trapping of hydrocarbons. The sand is especially clean and well sorted and therefore very porous and permeable.”

    The expedition, carrying an international team of 35 scientists from 14 countries, recovered 5km of core samples from an area along the Gulf of Cadiz and west of Portugal.

    The research found that a powerful cascade of Mediterranean water spilling into the Atlantic was scouring the rocky seafloor, carving deep-sea channels and building up mountains of mud. This is due to Mediterranean water being saltier than the Atlantic and therefore denser, causing it to plunge downwards.

    Dr Hernandez-Molina added: “We set out to understand how the Strait of Gibraltar acted first as a barrier and then a gateway over the past six million years. The fascinating results we came back with have hugely increased our understanding of the Mediterranean Outflow Water (MOW) that flows through the Gibraltar gateway and have led to some key discoveries about the relationship between climatic shifts, deep-water circulation and plate tectonic events over a huge timescale.”

  • An Early Double Dissolution? Don’t Hold Your Breath!

    10 Jun 2014
    Home  »  Uncategorized   »   An Early Double Dissolution? Don’t Hold Your Breath!

    An Early Double Dissolution? Don’t Hold Your Breath!

    Posted in Uncategorized By Neville On June 10, 2014

    Home  »  Uncategorized   »   An Early Double Dissolution? Don’t Hold Your Breath!

    An Early Double Dissolution? Don’t Hold Your Breath!

    Posted in Uncategorized By Neville On June 3, 2014

    Hold Your Breath!

    An Early Double Dissolution? Don’t Hold Your Breath!

    Posted in Uncategorized By Neville On May 27, 2014

    « JSCEM Recommends Optional Preferential Voting for the Senate | Main | Queensland set for another By-Election »

    May 19, 2014

    An Early Double Dissolution? Don’t Hold Your Breath!

    The tedious topic of a double dissolution seems to be doing the rounds again. In particular, there seems to be quite a lot of badly informed commentary on political blog sites on how a double dissolution would be brought on.

    Let me quote one website commentator who manages to encapsulate these misunderstandings in two sentences.

    “There will be a DD in early 2015 whether Abbott wants it or not (he very unlikely to want it as by then 2PP polling will be something like 60-40 against him!). Shorten will deny him supply, and rightly so.”

    This comment is wrong for two fundamental constitutional reasons. First, a Prime Minister may choose to call a double dissolution election but they cannot be forced to call one. Second, you cannot get a double dissolution from blocking a supply bill, though a government may choose to call a double dissolution on other grounds because supply is blocked.

    So let me go through the mechanism of a double dissolution and also clear up this issue with supply bills.

    The key point to make is that a double dissolution of the House and the whole Senate, followed by an election and possibly a joint sitting, is a significant constitutional event, not some euphemism for an early election.

    The double dissolution mechanism is set out in section 57 of the Constitution. It was drafted and endlessly debated in the 1890s constitutional conventions. It was a constitutional mechanism that allowed a government with a majority in the House of Representatives to overcome the blocking power of the Senate.

    The need for some method to resolve deadlocks between the House and Senate was created by the decision to give the Senate virtually co-equal powers with the House, something that was unworkable under the Westminster model of responsible government unless a deadlock provision was provided.

    As it was envisaged, Section 57 was a mechanism that would allow the population of the larger states as represented by the majority government in the House of Representatives to overcome the blocking power of the smaller states in the Senate. While the Senate never became the state assembly imagined by the constitutional drafters, the double dissolution power was still an important mechanism and has been used six times.

    The double dissolution power is unique to the Commonwealth constitution. It was a power created for the Governor-General to use in their name, not as the representative of the Queen. It is a power created by the Constitution and is not a reserve power inherited from the British Monarch.

    Putting the double dissolution mechanism in dot points, it consists of the following steps –

    • A bill must first pass the house and then be rejected, fail to pass or be unacceptably amended by the Senate.
    • After a period of three months, the bill may be re-presented to the House. After its passage through then House, if it is again rejected, fails to pass or is unacceptably amended by the Senate, then the legislation has become a ‘trigger’ for a double dissolution.
    • The Prime Minister may choose to use one or more triggers as ground for a double dissolution of both chambers followed by an election for the House and the whole Senate. This is not allowed to take place in the last six months of the House’s term.
    • After the election the legislation must be presented to the new House, and after its passage, must be presented to the new Senate.
    • If the Senate again rejects, fails to pass or unacceptably amends the legislation, then the Prime Minister can request that the Governor-General summon a joint sitting of the two chambers sitting and voting as one on the legislation. At the joint sitting, a simple majority of those members and senators present can pass the legislation which is then signed into law by the Governor General. A legislative (as opposed to ceremonial) joint sitting cannot occur without a double dissolution election having first taken place, and no other legislation can be considered at a joint sitting.

    The originally drafted Section 57 contained a requirement that three-fifths support was required for a bill to pass at a joint sitting. This was part of the draft constitution that failed to pass in NSW at the 1898 referendum. NSW Premier George Reid had the provisioned weakened to requiring a simple majority, one of several changes that strengthened the power of the Commonwealth government and the power of the larger states and led to the acceptance of the Constitution at a second referendum in 1899.

    This mechanism can be used for normal legislation but is almost impossible to be used in relation to appropriation and supply bills.

    The term ‘supply’ has a specific meaning for the parliament, but in its common use means the main Appropriation Bills that sets out how much money has been set aside for the normal working of each department in the next 12 months.

    The current appropriation bills were introduced with the budget speech last Tuesday. They specify how much money each government department can spend between 1 July 2014 and 30 June 2015. These bills are in the process of passing the House, will soon go to the Senate, and have to be passed by by both houses before 30 June this year or government will cease to function on 1 July.

    That is why the blockage of the Appropriation bill cannot be a trigger for a double dissolution. As currently formulated, it is not possible for the Appropriation bills to be defeated and the parliament come back and debate them again in three months time. The government would have run out of money by then.

    Budgets usually include other pieces of legislation covering detail of the budget. For instance the current budget will require legislation or regulation changes that cover pensions, tax rates, Medicare and the like. Any legislation of this type could be used as a double dissolution trigger after a second blockage, though regulation disallowance couldn’t. Oppositions tend to be selective in deciding which budget measures to oppose, the least popular measures being least likely to become double dissolution triggers.

    Unless there is other legislation that the government can use as a trigger to obtain a double dissolution, the blockage of supply can only force a House of Representatives election. There is no ability for the blockage of Appropriation bills as currently formulated to be used as a double dissolution trigger.

    So what happened to produce double dissolutions in 1974 and 1975 following the blockage of budget bills?

    The answer is that both of those double dissolutions had a background in the blockage of supply or appropriation bills, but in both cases it was triggers created by other blocked legislation that permitted double dissolutions to take place.

    A key point of difference between today and the Whitlam government is the timing of the budget. Today the budget is in May and the appropriation bills cover the whole of the next financial year. Until the mid-1980s the budget was in August, and what is more correctly known as a ‘supply’ bill was passed in May to authorize government expenditure between 1 July and 30 November, pending the passage of the budget.

    In 1974 it was the blockage of the interim supply bill that saw Gough Whitlam advise for a double dissolution based on six other pieces of legislation. Whitlam warned the Senate he would do this if it blocked supply, and the holding of the election was made easier as the election replaced an already announced separate half-Senate election.

    In 1975, the Opposition controlled Senate deferred the passage of the budget bills, demanding the government first announce the holding of an election. The government had interim supply to get it through to 30 November, perhaps longer if it saved money on its spending.

    In the end the Governor-General Sir John Kerr intervened to resolve the on-going deadlock before the supply period ran out. He appointed Opposition Leader Malcolm Fraser as Prime Minister, who promptly authorized his Senate members to pass the budget, and then requested a double dissolution based on other Whitlam government legislation. The subsequent Fraser government made no attempt to revive the legislation used as the basis for the double dissolution.

    If the budget bills had not been passed by the Senate on 11 November 1975, then Kerr and Fraser would have been in a very messy constitutional pickle by being unable to fund the holding of an election. But that is a scenario for alternative histories rather than relevant to today.

    For historical reasons I do not believe the Labor Party will even consider blocking the appropriation Bills. The Labor Party has demonized conservative controlled upper houses that blocked supply against Labor governments in Tasmania in 1925 and 1947, the Cain Labor government in Victoria in 1947, and the Whitlam government in 1974 and 1975.

    That using upper houses to block supply and bring on an election is a last resort weapon can be shown by the reticence of Coalition controlled Legislative Councils in the early 1990s to block supply and bring down the Lawrence Labor government in WA or Kirner Labor government in Victoria.

    The only time the Labor Party has voted against supply in an upper house in a situation where it would bring down a government was in Victoria in 1952, and that was a much more complex case involving a government that also lacked a lower house majority.

    But let me assume for a moment that the Labor Party would go against its history and vote with the Greens in the Senate to defeat the Appropriation Bills. What happens next?

    First, if the government chose to call an election of any sort, an interim supply bill would have to be passed allowing government to continue functioning from 1 July until a new parliament could convene.

    When the Hawke government announced its intention to call a double dissolution election for early July 1987, it had to continue with the sitting of parliament until supply had been passed to cover the period until after the election.

    But what election could the government call? At this stage the only option is for a separate House election. There couldn’t be a half-Senate election and there could not be a double dissolution because no trigger exists that would permit Section 57 to come into play.

    There are several pieces of legislation concerning the repeal of the Gillard’s climate change legislation that could become triggers in the near future. (You can see a full list of possible future triggers via this link.)

    Of these bills, the only one that has passed back through the House and been re-presented to the Senate is the Clean Energy Finance Corporation (Abolition) Bill 2013. If this were defeated in the next month, it would permit the calling of a double dissolution once interim supply was arranged.

    But using this bill as a double dissolution trigger would be the Prime Minister’s choice. If supply was blocked and the government was forced to an election, the Prime Minister could call a House election. Even if the Prime Minister had a double dissolution trigger, it is his choice to use it. The government can be forced to an election but it can’t be forced to a double dissolution.

    But two final political points also need to be kept in mind.

    First, any attempt to hold a double dissolution under the Senate’s current electoral system would be almost impossible. There would be even more parties and candidates contesting given the near halving of the quota for election. There will not be another election until changes are made to the Senate’s electoral system. Those changes can be legislated quickly but will need time to be implemented before an election can be held.

    A second political point is that the Abbott government’s budget is not the sort of budget you introduce if you desire an early election. It is the classic tough first term budget introduced in the hope that in three years time the anger will have subsided and the economy and budget would be in a better position.

    So everyone should just calm down and understand that in all likelihood the current government will be in place until the second half of 2016.

    Even if the government gets multiple double dissolution triggers, it will not use those triggers unless it thinks it can win the subsequent election.

    It is noteworthy that having floated the idea of a double dissolution last week, the government has quickly talked down the suggestion.

    In my opionion there is not going to be a double dissolution in the near future, and even in the more distant future, I cannot see any possibility of a double dissolution before late 2015 or the first months of 2016. Even then, a double dissolution will not occur unless the government thinks it will win.

    Posted by on May 19, 2014 at 02:28 PM in Double Dissolutions,

  • Daily update: Clean energy trends that Australia chooses to ignore

    1 of 6
    Why this ad?
    $2990 3kw solar systemwww.dollarsolar.com.au – $3990 for a 5kw solar power system $9980 for a 10kw solar power system

    Daily update: Clean energy trends that Australia chooses to ignore

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    Renew Economy editor@reneweconomy.com.au via mail74.atl111.rsgsv.net

    1:43 PM (8 minutes ago)

    to me
    Clean energy trends that Australia chooses to ignore, “World first” solar roof with heat and power, Coal not bedrock of Hunter Valley economy, Solar’s time to rise and shine, Hybrid storage inverters to seal the deal for solar, Carbon laws are working like them or not, Fiddling with tariffs could be death of utilities, What is Google plotting for the smart grid? and Buffett to double $15bn bet on renewables.
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    RenewEconomy Daily News
    The Parkinson Report
    Tony Abbott’s new climate goal may be a 30% cut in reputation. If so, he has certainly achieved that already, but he could be causing more fundamental problems for the Australian economy.
    Bluescope unveils “world first” built-in solar array that generates electricity and heat, and acts as roofing.
    Two new assessments puncture the myth that the coal industry is major contributor to jobs and growth in Hunter Vally and US.
    Photovoltaic efficiency records are being shattered, thanks to recent advances in materials science. Its time for solar to shine.
    Grid operators and supportive governments may try and stymie solar, but the new wave of battery hybrids means the horse has already bolted.
    Australia’s carbon laws are about to turn 2 – pollution is down, the economy is up, scare campaigns exposed, wind and solar grow
    Utilities need to shift the conversation to look at total value proposition for customers, or solar and storage will take their business models.
    Google is developing secret power grid plan based around energy software and hardware, and led by clean-tech guru  Arun Majumdar.
    Warren Buffett is looking to invest another $15 billion in renewable energy, judging by recent comments by the mega-investor.