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  • Elucidating Heavy Precipitation Events

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    Elucidating Heavy Precipitation Events

    Nov. 29, 2013 — It is difficult to forecast heavy precipitation events accurately and reliably. The quality of these forecasts is affected by two processes whose relative importance has now been quantified by a team at the Laboratoire d’Aérologie (CNRS / Université Toulouse III-Paul Sabatier). The researchers have shown that these processes should be taken into account in low wind speed events. Their findings should help forecast these events, which repeatedly cause significant damage, especially in south-eastern France. They are first published online the November 28, 2013 in the Quarterly Journal of the Royal Meteorological Society.


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    Nearly every autumn, the countries of the Mediterranean Basin are stricken by heavy rainfall and flash floods, which endanger populations and can cause significant property damage. South-eastern France is frequently affected by these events, caused by the interaction between topography and the still warm and moisture-laden air masses from the Mediterranean Sea. Weather forecasters are able to predict these events and issue weather warnings. However, simulating their evolution on different time scales remains difficult, just like forecasting the strength and location of precipitation, the two parameters that broadly determine the extent of flooding.

    Researchers from CNRS and Université Toulouse III-Paul Sabatier at the Laboratoire d’Aérologie investigated two phenomena that play a key role in meteorology: the microphysics of hydrometeors (rain, snow and ice pellets)[1] and atmospheric turbulence. The aim was to determine the relative effect of these two processes on forecast sensitivity. To do this, the scientists looked at five heavy rainfall episodes that took place between September 2010 and November 2011 in south-eastern France and for which measured data was available. For each event, ensemble simulations were carried out using the Meso-NH[2] atmospheric research model, giving more or less importance to each of the two processes.

    Two main results emerged. For high wind speed events, precipitation is scarcely affected by the perturbations introduced. It is therefore unnecessary to take account of these two processes to improve heavy precipitation forecasting. In this case, it is the interaction with the topography that determines the onset of precipitation. However, when wind speed is low, both the intensity of precipitation and its location (upstream of the topography) are far more sensitive to these two processes. In this case, the microphysics of hydrometeors and atmospheric turbulence need to be better represented so as to improve forecast sensitivity.

    These results suggest that in low wind speed situations, errors related to the representation of microphysical and turbulent processes make a significant contribution to the total error in the forecasting system. Taking greater account of these errors would improve heavy precipitation forecasting when wind speed is low. The study was also used to test a methodology that may be implemented as part of the HyMeX[3] international research program, launched in 2010 for a period of ten years and coordinated by Météo-France and CNRS.

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    The above story is based on materials provided by CNRS (Délégation Paris Michel-Ange).

    Note: Materials may be edited for content and length. For further information, please contact the source cited above.


    Journal Reference:

    1. A. Hally, E. Richard, S. Fresnay, D. Lambert. Ensemble simulations with perturbed physical parametrizations: Pre-HyMeX case studies. Quarterly Journal of the Royal Meteorological Society, 2013; DOI: 10.1002/qj.2257

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    CNRS (Délégation Paris Michel-Ange) (2013, November 29). Elucidating heavy precipitation events. ScienceDaily. Retrieved November 30, 2013, from http://www.sciencedaily.com­ /releases/2013/11/131129101903.htm?utm_source=feedburner&utm_medium=email&utm_campaign=Feed%3A+sciencedaily%2Fearth_climate%2Fsevere_weather+%28ScienceDaily%3A+Earth+%26+Climate+News+–+Severe+Weather%29

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  • How will Australia cope with the housing demands of a doubled population?

    How will Australia cope with the housing demands of a doubled population?

    By Cameron Kusher
    Friday, 29 November 2013

    The Australian Bureau of Statistics (ABS) released national population projections earlier this week.  The data looks at the projected growth in the national population from 2012 through to 2101 and the data provides a fascinating insight into the potential future of Australia over the coming years and decades.

    The projections look at three different scenarios which can be read about here.  For the purposes of this post we are utilising ‘Series B’ or the medium level projections.  Based on this series, Australia’s population was estimated to be 22,721,995 persons in 2012, by 2101 the population is projected to be 136% higher at 53,564,333 persons.  Under this scenario we would see the national population from 2012 having doubled by 2071.  Keep in mind Australia was first settled by Europeans in 1788 so it took 224 years to get to the 2012 population and it projected to double in just 59 years.Projections are also provided at a state and capital city level from 2012 through to 2061, at which time the national population is projected to be 41,513,375.

    state by state

    The above table details the estimated population as at June 2012 and the percentage of the national population across each state and compares it to the same projected data for 2061 as well as showing the average annual growth rate over the period.  At a state level, the proportion of the national population is projected to fall in New South Wales, South Australia, Tasmania and Northern Territory.  The proportion is projected to remain static in Victoria and rise across Queensland, Western Australia and the Australian Capital Territory.  Western Australia (2.0%), Queensland (1.5%) and the Australian Capital Territory (1.4%) are projected to record the greatest average annual rate of population growth while Tasmania (0.2%), South Australia (0.7%) and New South Wales (0.9%) are projected to record the lowest growth rate.

    Of course these are just population projections and are no way set in stone however, it does seem inevitable that the population of the country will expand substantially (even based on the low series of assumptions) over time.  The big question remains where and how will we house all of these additional citizens? Based on the data provided in the release it seems that a significant majority of the population will continue to live within our capital cities.

    cap city by cap city

    The above table details the estimated population as at June 2012 and the percentage of each state’s population across each capital city and compares it to the same projected data for 2061 as well as showing the average annual growth rate over the period.

    There are quite a few interesting points to take from these long-term projections.  Firstly, by 2061 Sydney will no longer be the nation’s most populous city and Brisbane will no longer be the nation’s third most populous city.  Melbourne will overtake Sydney as the most populous city in 2053 and Perth will overtake Brisbane as the third most populous city in 2028.

    The proportion of Australian’s living within a capital city is already quite high at 66.1% however, this is projected to increase to 73.4% by 2061.  Think about that, out of a projected population of 41.5 million, almost three out of every four Australians will live in a capital city.  If we focus on the four most populous capital cities, 57.3% of Australians currently live in Sydney, Melbourne, Brisbane or Perth.  Based on the population projections, by 2061 65.8% of the total national population will live in Sydney, Melbourne, Brisbane and Perth.

    Should this scenario actually come to fruition it will create significant challenges for each of these cities.  Obviously housing is a challenge which immediately comes to mind, how and where these people can be housed and what it would mean for property values.  Over time the capital city areas do expand however, for a city such as Sydney that is surrounded by water and national parks the scope to expand is quite limited. No wonder the inner city areas are undergoing such rapid densification.

    Elsewhere you can continue to grow the urban sprawl but there must be a consideration around how people travel around the city and commute to their jobs.  Transport infrastructure is typically already insufficient, without appropriate investment levels how much worse would it be by 2061?  Of course, for some, purchasing a home in a capital city is already out of reach; how do governments ensure that a greater number and proportion of capital city residents doesn’t just lead to further escalation of property values?

    Of course these figures are in no way set in stone however, it does appear that the country’s population will continue to grow which will pose myriad challenges.  In my opinion the greatest concern is the projection of a greater centralisation of the population to our capital cities and more pointedly the four most populous cities.

    As mentioned, in each of these cities there are already affordability barriers for certain home buyer cohorts and investment in transport infrastructure has not been sufficient.  In my opinion we should be looking to a decentralisation of the population rather than encouraging more and more people to the capital city.  Not only do regional markets tend to have lower house values, in many instances they offer a superior lifestyle than that which is available within our major capital cities.

    The biggest challenge of course is employment in regional areas however, with the advent of high speed internet and major infrastructure projects such as the National Broadband Network (NBN) we will hopefully see the nature of work change with more telecommuting taking place and less focus on physically being located within an office.

    Alternatively, many businesses do not necessarily need to be located within a major capital city.  Perhaps governments could incentivise major businesses to locate their headquarters or major offices outside of Sydney, Melbourne, Brisbane or Perth.

     


    Cameron Kusher is senior research analyst at RP Data.

  • ‘Black Friday’ Originally Meant Something Much, Much Darker

    Edition: U.S.

     

    ‘Black Friday’ Originally Meant Something Much, Much Darker

    The Huffington Post  |  By Posted: 11/27/2013 8:15 am EST  |  Updated: 11/27/2013 5:11 pm EST

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    It’s totally understandable if you think the term “Black Friday” is a direct linguistic descendent of “in the black,” accounting jargon for turning a profit. After all, the day after Thanksgiving is now one of the biggest shopping days of the year, an annual delight to retailers hoping to give their bottom lines a nice little boost in the year’s final weeks.

    But the truth is that Black Friday owes its name to the Philadelphia Police Department, which did not have profitability in mind. One thing to remember is that, long before the rest of us started calling it Black Friday, retailers hoped to start the holiday shopping season with a bang by offering “can’t miss” deals right after Thanksgiving. (Note: These days, “holiday shopping season” can begin way before Turkey Day.) People being people, they have long stormed stores, caused traffic jams and been generally terrible to one another in an effort not to miss these deals.

    In the middle years of the twentieth century, the scene was often particularly bad in Philadelphia, where the annual Army-Navy football game was regularly played on the weekend after Thanksgiving.

    Lots of cars, lots of traffic, lots of chaos. Sound familiar?

    So at some point in the 1950s or 1960s — some put the date exactly at 1966 — the Philadelphia Police Department started to refer to the day after Thanksgiving as “Black Friday,” with the unrealistic hope that people would find the whole shebang distasteful and opt out of the collective consumer madness. At a minimum, it was a derisive way to describe an unpleasant day in the life of a Philly cop.

    “It was not a happy term.” retail scholar Michael Lisicky told CBS Philly in 2011. “The stores were just too crowded, the streets were crowded, the buses and the police were just on overcall and extra duty.”

    The term took off in a big way, but not for the reasons the cops hoped. By the 1980s, the idea gained steam that “Black Friday” was named after retailers trying to hop into the black, according to The Telegraph.

    Then, somewhere along the way, Corporate America joyfully co-opted the phrase for their own use

  • Ocean acidification in the Bay of Bengal

    Ocean acidification in the Bay of Bengal

    Published 28 November 2013 Science 1 Comment
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    The present study dealt with acidification of the Bay of Bengal and its impact on marine environment. It revealed that the average pH value of water in the Bay of Bengal on an average was around 7.75. The study showed strong positive correlation between pH and bicarbonate (R2 is 0.930), between electric conductivity and salinity (R2 is 0.999) and between electric conductivity and dissolved oxygen (R2 is 0.999). The pH in the Bay of Bengal has fallen by 0.2 units between 2012 and 1994 (pH 7.95). The study infers an impact of reduction of pH on calcifying organisms such as sea shells, oyster and coral reefs that are playing essential roles in their respective ecosystems. Average calcium carbonate composition of the calcifying organisms was found to be 80% which was 17% lower than the standard composition. The lower pH (7.75) might have made the Mollusks vulnerable and fragile which was evidenced by the presence of lesser number of Mollusks compared to that of 5 to 6 years back.

     

    Rashid T., Hoque S. & Akter F., in press. Ocean acidification in the Bay of Bengal. Open Access Scientific Reports. Article.

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  • Global ocean currents explain why Northern Hemisphere is the soggier one

    28Nov

    Global ocean currents explain why Northern Hemisphere is the soggier one

    A quick glance at a world precipitation map shows that most tropical rain falls in the Northern Hemisphere. The Palmyra Atoll, at 6 degrees north, gets 175 inches of rain a year, while an equal distance on the opposite side of the equator gets only 45 inches. Scientists long believed that this was a quirk of the Earth’s geometry – that the ocean basins tilting diagonally while the planet spins pushed tropical rain bands north of the equator. But a new University of Washington study shows that the pattern arises from ocean currents originating from the poles, thousands of miles away.

    The findings, published in Nature Geoscience, explain a fundamental feature of the planet’s climate, and show that icy waters affect seasonal rains that are crucial for growing crops in such places as Africa’s Sahel region and southern India.

    In general, hotter places are wetter because hot air rises and moisture precipitates out.

    “It rains more in the Northern Hemisphere because it’s warmer,” said corresponding author Dargan Frierson, a UW associate professor of atmospheric sciences. “The question is: What makes the Northern Hemisphere warmer? And we’ve found that it’s the ocean circulation.”

    Frierson and his co-authors first used detailed measurements from NASA’s Clouds and Earth’s Radiant Energy System, or CERES, satellites to show that sunlight actually provides more heat to the Southern Hemisphere – and so, by atmospheric radiation alone, the Southern Hemisphere should be the soggier one.

    After using other observations to calculate the ocean heat transport, the authors next used computer models to show the key role of the huge conveyor-belt current that sinks near Greenland, travels along the ocean bottom to Antarctica, and then rises and flows north along the surface. Eliminating this current flips the tropical rain bands to the south.

    The reason is that as the water moves north over many decades it gradually heats up, carrying some 400 trillion (that’s four with 14 zeroes after it) watts of power across the equator.

    For many years, slanting ocean basins have been the accepted reason for the asymmetry in tropical rainfall.

    “But at the same time, a lot of people didn’t really believe that explanation because it’s kind of a complicated argument. For such a major feature there’s usually a simpler explanation,” Frierson said.

    The ocean current they found to be responsible was made famous in the 2004 movie “The Day After Tomorrow,” in which the premise was that the overturning circulation shut down and New York froze over. While a sudden shutdown like in the movie won’t happen, a gradual slowing – which the recent United Nations report said was “very likely” by 2100 – could shift tropical rains south, the study suggests, as it probably has in the past.

    The slowdown of the currents is predicted because increasing rain and freshwater in the North Atlantic would make the water less dense and less prone to sinking.

    “This is really just another part of a big, growing body of evidence that’s come out in the last 10 or 15 years showing how important high latitudes are for other parts of the world,” Frierson said.

    Frierson’s earlier work shows how the changing temperature balance between hemispheres influences tropical rainfall. A recent study by Frierson and collaborators looked at how pollution from the industrial revolution blocked sunlight to the Northern Hemisphere in the 1970s and ’80s and shifted tropical rains to the south.

    “A lot of the changes in the recent past have been due to air pollution,” Frierson said. “The future will depend on air pollution and global warming, as well as ocean circulation changes. That makes tropical rainfall particularly hard to predict.”

    ###

    Co-authors of the paper are Yen-Ting Hwang, Elizabeth Maroon, Xiaojuan Liu and David Battisti at the UW; Neven Fuckar at the University of Hawaii; Richard Seager at Columbia University; Sarah Kang at South Korea’s Ulsan National Institute of Science and Technology; and Aaron Donohoe at the Massachusetts Institute of Technology.

    The research was funded by the National Science Foundation, the Japan Agency for Marine-Earth Science and Technology, the National Aeronautic and Space Administration, the National Oceanic and Atmospheric Administration and the U.S. Department of Defense.