Sunday, March 22, 2009

The Last Girl In School

As school began again this year, Anita Chaudhary was prepared to spend back-to-school day as she had for the last few years: at home. She was certain that, once again, she'd watch from the doorway of her family's tiny house as dozens of neighbor children passed by on their way to class.
Photo: Thatcher Cook for Mercy Corps Her family — mother, father and five children including herself — is perhaps the poorest in the village of Bichpuri, Nepal. Their garden plot, leased from the local landlord, is meager: perhaps the length and width of an average residential driveway in the United States. The Chaudhary family depends on the vegetables they grow here for year-round sustenance. There is nothing left to sell for additional household income.
Anita's father finds work when he can, mostly as a day laborer for local farmers during planting and harvest seasons. At other times of the year, it's nearly impossible for him to earn a regular wage: as a member of the area's Tharu ethnic group, he is looked down upon, an outcast.
Today, as always, 12-year-old Anita was up by 6 A.M. to help her mother with the morning chores: feeding the cows, washing the dishes and cleaning the house. Her father had left before sunrise to seek work for the day. But instead of tending the garden, by 7 A.M. she is dressed in a crisp, clean uniform, on her way to a morning study group. From there, she would walk with her friends to school in the neighboring village.
It turns out — thanks to her fellow youth in Bichpuri — that this year would be unlike any other for Anita. This year, she wouldn't be the one left behind.
Seeing a need
For the past few years, many members of Bichpuri's village youth council had walked by Anita's house on their way to school and seen the lonely girl standing there, glancing from her doorway.
"She was the only person her age in the village not attending school," said 21-year-old Uday Raj Chaudhary, president of the council. "Everyone should have the opportunity to learn. So our group met and decided to do something."
Uday and the other 48 members of the council — whose ages range from 16 to 30 — discussed the situation, pooled their own money and sent representatives to speak with Anita's family. They offered to pay the 500 Nepalese rupee ($7.00) enrollment and 300 rupee ($4.22) monthly tuition, as well as the cost for uniforms and other fees. Anita's mother and father happily accepted.
Public school in Nepal is supposed to be essentially free of cost. However, a lack of government resources has led to overcrowded classrooms and an unmanageable teacher-to-student ratio. The school that Anita attends has 500 students, but only 15 teachers. As a result, communities bear the cost of hiring additional teachers for local schools — fees that are often passed on to poor families who can't afford to spend any more.
Children in many neighboring villages aren't as fortunate as Anita and remain at home as she once did.
Better late than never
Anita attends school from 10 A.M. to 4 P.M. six days a week, Sunday through Friday. Her classes include social studies, history, Nepali language, and science. Her favorite course is math. Why?
"Because I'm good at it," she smiled, shyly.
She missed three years of school, so Anita is in third grade, in class with nine- and ten-year-olds. Nevertheless, she is making the best of her opportunity.
"She is a very hard worker," said Uday. "She also helps other students with their work."
Helping is something that Anita aspires to make a career: she wants to continue in school and become a nurse.
"I would like to stay here in my village and care for the people here who fall ill," she explained. "I am happy to have the chance to go to school now. I'm glad that my friends here put their trust in me, and I will always remember their kindness."

Famous paleontologist to plead guilty to fossil theft

An internationally renowned paleontologist will plead guilty to stealing dinosaur bones from federal land, his attorneys said in a court filing.
Nate Murphy, whose famous finds include Leonardo, one of the best-preserved dinosaurs in the world, will make that plea in federal court in Billings, Montana.
Earlier this month, Murphy pleaded guilty to state charges of stealing a fossil from private land in order to sell it. An expert cited in that case said Murphy's find was worth between $150,000 and $400,000.
The self-taught dinosaur expert, who is director of vertebrate paleontology at the Judith River Dinosaur Institute, could face jail time.
Murphy and his attorney did not immediately respond to phone messages Friday from CNN.
Jessica Fehr, lead prosecutor in the case, said the U.S. Attorney's Office would not comment until after the plea is entered.
In court papers, federal prosecutors say Murphy knowingly took fossils from federal property between about August 2006 and August 2007. The "paleontological resources" were said to be worth at least $1,000.
In the state case, Murphy pleaded guilty to a felony charge of theft. As part of the plea, the state recommended Murphy's sentence be deferred for five years.
Douglas Erwin, president of The Paleontological Society and curator of the Smithsonian's National Museum of Natural History, said "theft of fossils from pubic lands has long been a problem."
In a written statement sent to CNN on Friday, he said such thefts "can often result in the loss of important scientific information and the disappearance of specimens that belong to the public.
"At the same time, however, fossil collecting, particularly of common invertebrate fossils, has been a pastime enjoyed by many for decades, and is an important way of connecting people with their natural heritage."

Legacy of the great Chinese plant takeaway

As you read this, a spring tide of colour is advancing across a certain Chinese hillside. The rhododendrons and camellias are getting into their stride; the stream that tumbles down its slopes to spread out at the feet of a little butterfly-roofed pavilion will soon be half-hidden by clumps of primula and, later, iris. Plant aficionados would kill to get their gardening gloves on some of these rarities. Or be killed.
Yet the only special thing about this little hill is that it overlooks the rooftops of Edinburgh. Its flora pay tribute to the Scottish plant collectors whose intrepid explorations changed the face of the herbaceous border and continue to enrich the Royal Botanic Garden Edinburgh (RBGE) with the largest collection of wild-origin Chinese plants outside China.
Many of their labels bear the name of George Forrest, Scotland's horticultural Indiana Jones, who set off on his first expedition into the remote mountainous region of Yunnan, in south-west China, on May 14, 1904 - an event now being celebrated with an exhibition at the RBGE. George Forrest - A Life and Legacy draws upon 1,700 glass-plate negatives and original prints taken by Forrest and often developed in the field, along with letters, artefacts and a newly discovered film. This month also sees the publication of Brenda McLean's biography, George Forrest, Plant Hunter, which colourfully retraces the botanist's footsteps in China.
I wish I had known more about George Forrest when I visited Lijiang, declared a World Heritage Site in 1996 when an earthquake exposed the frailty and beauty of a town elevated to soap-style stardom by the book and BBC documentary Beyond the Clouds. I missed out on the lilies of the field, being entirely mesmerised by the people working there, the Naxi women dressed for the rice paddies like medieval princesses.
A hundred years ago, an altogether less pampered experience than mine lay ahead of George Forrest, a 31-year-old herbarium assistant, who set off with the blessing of the RBGE to make his way to present-day Tengchong by paddleboat, mule and on foot. It was to be the start of a 28-year love affair with the spectacular Cang Shan and Yulong Xue Shan ranges, known then as the Tali and Lichiang mountains.
A plant-hunting traveller's lot was no picnic. The hundreds of letters underpinning McLean's biography recount hardship and insecurity, homesickness and howling wolves. In the summer of 1905, Forrest had to flee for his life from warring Tibetan lamas who had sacked the mission at Tsekou and murdered his two missionary friends. Disguised as a local, he hid in the hills for 21 days.
"About 20 natives were killed and a great many more captured and taken into slavery," he wrote back to his sponsor at the RBGE. "The heads and hearts were taken north to Atunze … but I was lucky." The sack of Tsekou resulted in the loss of 770 specimens and seeds, plus his camera and negatives - a whole season's work.
By the time Forrest died in 1932, he had made seven expeditions to Yunnan. More than 30,000 of his specimens are preserved in the RBGE herbarium - the core of a legacy that was to give horticulture a whole new palette and botanists an introduction to a rich and unique flora. British gardens would never look the same again; we owe many now-familiar species of primula, rhododendron, iris, camellia, clematis, gentian, jasmine and conifer to George Forrest's exploits.
May is the best time to visit Edinburgh's serene and beautiful botanic gardens. After Oxford's, they are the oldest in Britain and regarded as one of the top five in the world in terms of diversity and global outreach. The approach here is practical and contemporary, with children's events, workshops, craft classes and controversial exhibitions of modern art taking place both outdoors and indoors.
With gardening now ranking second only to reading among Britain's favourite leisure pursuits, visitor numbers are booming, says Clara Govier of the RBGE. Last year, 706,000 passed through the gates - up 12 per cent on the previous year. Growth in the short-break market has lengthened the season so much that the RBGE's satellite garden at Dawyck, near Peebles, is looking to extend its 2005 programme to include February and November. Small operators offering garden tours, both at home and abroad, are also experiencing record interest.
Gardening, like tourism, has even had an impact on faraway Jade Dragon Snow Mountain, near Lijiang. Three years from now, a new botanic garden will open there under the auspices of the RBGE and its Chinese partners. Forrest was a pioneer in recognising the value of local expertise, recruiting collectors from among the ethnic minorities, especially the Naxi. But much of the uncharted landscape they traversed is now developed and deforested. Botanists at the RBGE want the new garden at Lijiang to be a model of sustainability, encouraging activities - including tourism - in a way that will help preserve the rich biodiversity of the area.

Friday, March 20, 2009

Wildfire: Behavior, Prevention, Detection and Supression

Wildfires are common in many places around the world, including much of the vegetated areas of Australia as well as the veld in the interior and the fynbos in the Western Cape of South Africa. The forested areas of the United States and Canada are also susceptible to wildfires. The climates are sufficiently moist to allow the growth of trees, but feature extended dry, hot periods. Fires are particularly prevalent in the summer and fall, and during droughts when fallen branches, leaves, and other material can dry out and become highly flammable. Wildfires are also common in grasslands and scrublands.
Wildfires tend to be most common and severe during years of drought and occur on days of strong winds. With extensive urbanization of wildlands, these fires often involve destruction of suburban homes located in the wildland urban interface, a zone of transition between developed areas and undeveloped wildland.
Today it is accepted that wildfires are a natural part of the ecosystem of wildlands, where plants have evolved to survive fires by a variety of strategies (from possessing reserve shoots that sprout after a fire, to fire-resistant seeds), or even encourage fire (for example eucalypts contain flammable oils in their leaves) as a way to eliminate competition from less fire-tolerant species. In 2004, researchers discovered that exposure to smoke from burning plants actually promotes germination in other types of plants by inducing the production of the orange butenolide. Most native animals, too, are adept at surviving wildfires.
On occasions, wildfires have caused large-scale damage to private or public property, destroying many homes and causing deaths, particularly when they have reached urban-fringe communities. Wildfires are extremely dangerous,but some are purposely caused.
BEHAVIOR
The evaporation of Deer fecis in plants are balanced by water absorbed from the soil. Below this threshold, the plants dry out and under stress release the flammable gas ethylene. A consequence of a long hot and dry period is therefore that the air contains flammable essences and plants are drier and highly flammable.
The propagation of the fire has three mechanisms:
"crawling" fire: the fire spreads via low level vegetation (e.g., bushes)
"crown" fire: a fire that "crowns" (spreads to the top branches of trees) can spread at an incredible pace through the top of a forest. Crown fires can be extremely dangerous to all inhabitants underneath, as they may spread faster than they can be outrun, particularly on windy days. (see Firestorm)
"jumping" or "spotting" fire: burning branches and leaves are carried by the wind and start distant fires; the fire can thus "jump" over a road, river, or even a firebreak. In Australian bushfires, spot fires have been documented "up to 10 km [aprox. 6 miles] ahead of the fire front" (Billing 1983).
The Nevada Bureau of Land Management identifies several different wildfire behaviors. For example, extreme fire behavior includes wide rates of spread, prolific crowning and/or spotting, the presence of fire whirls, or a strong convection column. Extreme wildfires behave erratically and unpredictably.
In southern California, under the influence of Santa Ana winds, wildfires can move at tremendous speeds, up to 40 miles (60 km) in a single day, consuming up to 1,000 acres (4 km²) per hour. Dense clouds of burning embers push relentlessly ahead of the flames crossing firebreaks without pause.
Propagation of the fire with a characteristic shape of a "pear"The powerful updraft caused by a large wildfire will draw in air from surrounding areas. These self-generated winds can lead to a phenomenon known as a firestorm.
French models of wildfires dictate that a fire's front line will take on the characteristic shape of a pear; the major axis being aligned with the wind. In the case of the fires in southeastern France, the speed of the fire is estimated to be 3% to 8% of the speed of the wind, depending on the conditions (density and type of vegetation, slope). Other models predict an elliptical shape when the ground is flat and the vegetation is homogeneous.
Another type of wildfire is the smouldering fire. It involves the slow combustion of surface fuels without generating flame, spreading slowly and steadily. It can linger for days or weeks after flaming has ceased, resulting in potential large quantities of fuel consumed and becoming a global source of emissions to the atmosphere. It heats the duff and mineral layers, affecting the roots, seeds and plant stems at the ground.
Since 1997, in Kalimantan and East Sumatra, Indonesia, there is a type of continuous smouldering fire on the peat bogs that burn underground for years without any supply of oxygen. The underground fire ignited new forest fire each year during dry season.
PREVENTION
For many decades the policy of the United States Forest Service was to suppress all fires. This policy was epitomized by the mascot Smokey Bear and was also the basis of parts of the movie Bambi. The policy began to be questioned in the 1960s, when it was realized that no new Giant Sequoia had been grown in the forests of California, because fire is an essential part of their life cycle. This produced the policy of controlled burns to reduce underbrush. This clears much of the undergrowth through forest and woodland areas, making travel and hunting much easier while reducing the risk of dangerous high-intensity fires caused by many years of fuel buildup.
The previous policy of absolute fire suppression in the United States has resulted in the buildup of fuel in some ecosystems such as dry ponderosa pine forests. However, this concept has been misapplied in a "one-size-fits-all" application to other ecosystems such as California chaparral. Fire suppression in southern California has had very little impact over the past century. The amount of land burned in 6 southern California counties has been relatively unchanged. In fact, fire frequency has been increasing dramatically over the past century in lock step with population growth. Urbanization can also result in fuel buildup and devastating fires, such as those in Los Alamos, New Mexico, East Bay Hills, within the California cities of Oakland and Berkeley between October 19 and 22, 1991, all over Colorado in 2002, and throughout southern California in October 2003. Homes designed without considering the fire prone environment in which they are built have been the primary reason for the catastrophic losses experienced in wildfires.
On average, wildfires burn 4.3 million acres (17,000 km²) in the United States annually. In recent years the federal government has spent $1 billion a year on fire suppression. 2002 was a record year for fires with major fires in Arizona, California, Colorado, and Oregon. A wildfireThe risk of major wildfires can be reduced partly by a reduction or alteration of fuel present. In wildland, reduction can be accomplished by either conducting controlled burns, deliberately setting areas ablaze under less dangerous weather when conditions are less volatile or physical fuel removal by removing some trees as is conducted in many American forests. Alteration of fuels, which involves reducing the structure of fuel ladders, can be accomplished by hand crews with chain saws or by large mastication equipment that shreds trees and vegetation to a mulch. Such techniques are best used within the wildland/urban interface where communities connect with wild open space. Prescribed burns in the backcountry, away from human habitations, are not particularly effective in preventing large fires. All the large catastrophic fires in the United States have been wind driven events where the amount of fuel (trees, shrubs, etc.) has not been the most important factor in fire spread.
People living in fire-prone areas typically take a variety of precautions, including building their homes out of flame-resistant materials, reducing the amount of fuel near the home or property (including firebreaks, their own miniature control lines, in effect), and investing in their own firefighting equipment.
Rural farming communities are rarely threatened directly by wildfire. These types of communities are usually located in large areas of cleared, usually grazed, land, and in the drought conditions present in wildfire years there is often very little grass left on such grazed areas. Hence the risk is minimized. However, urban fringes have spread into forested areas, for example in Sydney and Melbourne, and communities have literally built themselves in the middle of highly flammable forests. In Cape Town, the city lies on the fringe of the Table Mountain National Park. These communities are at high risk of destruction in bushfires, and should take extra precautions.
There are quite a few US states, Canadian provinces and many countries around the world that still use Fire lookouts as a means of early detection of forest fires. Some nations still using this system besides the US and Canada include: Australia, Israel, Latvia, Poland, France, Germany, Italy, Spain, Portugal, Brazil, Uruguay.
FIRE SUPRESSION
Wildland fire suppression is a unique aspect of firefighting. Most fire-prone areas have large firefighter services to help control bushfires. As well as the water-spraying fire apparatus most commonly used in urban firefighting, bushfire services use a variety of alternative techniques. Typically, forest fire fighting organizations will use large crews of 20 or more people who travel in trucks to the fire. These crews use heavier equipment to construct firebreaks, and are the mainstay of most firefighting efforts. Other personnel are organized into fast attack teams typically consisting of 5–8 people. These fast attack teams are helicoptered into smaller fires or hard to reach areas as a preemptive strike force. They use portable pumps to douse small fires and chainsaws to construct firebreaks or helicopter landing pads if more resources are required. Hand tools are commonly used to construct firebreaks and remove fuels around the perimeter of the fire to halt its spread, including shovels, rakes, and the pulaski, a tool unique to wildland firefighting. In the eastern United States, portable leaf blowers are sometimes used. In the western United States, large fires often become extended campaigns, and temporary fire camps are constructed to provide food, showers, and rest to fire crews. These large fires are often handled by 20 person hand crews, sometimes known as hotshot crews, specially organized to travel to large fires.
Fast attack teams, such as the Boise District BLM Helitack crew, are often considered the elite of firefighting forces, as they sometimes deploy in unusual ways. If the fire is on a particularly steep hill or in a densely wooded area, they may rappel or fast-rope down from helicopters. If the fire is extremely remote, firefighters known as smokejumpers may parachute into site from fixed-wing aircraft. In addition to the aircraft used for deploying ground personnel, firefighting outfits often possess helicopters and water bombers specially equipped for use in aerial firefighting. These aircraft can douse areas that are inaccessible to ground crews and deliver greater quantities of water and/or flame retardant chemicals. Managing all of these various resources over such a large area in often very rugged terrain is extremely challenging, and often the Incident Command System is used. As such, each fire will have a designated Incident Commander who oversees and coordinates all the operations on the fire. This Incident Commander is ultimately responsible for the safety of the firefighters and for the success of firefighting efforts.
Large fires are of such a size that no conceivable firefighting service could attempt to douse the whole fire directly, and so alternative techniques are used. In alternative approaches, firefighters attempt to control the fire by controlling the area that it can spread to, by creating "control lines", which are areas that contain no combustible material. These control lines can be produced by physically removing fuel (for instance, with a bulldozer), or by "backfiring", in which small, low-intensity fires are started, using a device such as the driptorch, or pyrotechnic flares known as "fusees", to burn the flammable material in a (hopefully) controlled way. These may then be extinguished by firefighters or, ideally, directed in such a way that they meet the main fire front, at which point both fires run out of flammable material and are thus extinguished.
Unfortunately, such methods can fail in the face of wind shifts causing fires to miss control lines or to jump straight over them (for instance, because a burning tree falls across a line, burning embers are carried by the wind over the line, or burning tumbleweeds cross the line).
The actual goals of firefighters vary. Protection of life (those of both the firefighters and "civilians") is given top priority, then private property according to economic and social value and also to its "defendibility" (for example, more effort will be expended on saving a house with a tile roof than one with a wooden-shake roof). In very severe, large fires, this is sometimes the only possible action. Protecting houses is regarded as more important than, say, farming machinery sheds, although firefighters, if possible, try to keep fires off farmland to protect stock and fences (steel fences are destroyed by the passage of fire, as the wire is irreversibly stretched and weakened by it). Preventing the burning of publicly owned forested areas is generally of least priority, and, indeed, it is quite common (in Australia, at least) for firefighters to simply observe a fire burn towards control lines through forest rather than attempt to put it out more quickly; it is, after all, a natural process. On any incident, ensuring the safety of firefighters takes priority over fire suppression. When arriving on a scene a fire crew will establish a safety zone(s), escape routes, and designate lookouts (known by the acronym LCES, for lookouts, communications, escape routes, safety zones). This allows the firefighters to engage a fire with options for a retreat should their current situation become unsafe. In addition all fire suppression activities are based from an "anchor point" (such as lake, rock slide or road). From an anchor point firefighters can work to contain a wildland fire without the fire outflanking them. As a last resort, all wildland firefighters carry a fire shelter. In a unescapable burnover situation the shelter will provide limited protection from radiant and convective heat, as well as superheated air. As such a greater emphasis is placed on safety and preventing entrapment, and is reinforced with a list of 10 fire orders and 18 "watch out situations" for firefighters to be aware of, which warn of potentially dangerous conditions.
In North America, the belief that fire suppression has substantially reduced the average annual area burned is widely held by resource managers and is often thought to be self-evident. However, this belief has been the focus of vocal debate in the scientific literature. A new material called "gel" (made from super-absorbent polymer) is used in California, USA for fighting forest fire. Water is soaked up by the gel and stored in layers of tiny bubbles. The gel can protect tree/house for longer time than ordinary water, because it gets boiled by the fire one layer at a time.
ATMOSPHERIC EFFECTS
Most of the Earth's weather and air pollution reside in the troposphere, the part of the atmosphere that extends from the surface of the planet to a height of between 8 and 13 kilometers. A severe thunderstorm or pyrocumulonimbus in the area of a large wildfire can have its vertical lift enhanced to boost smoke, soot and other particles as high as the lower stratosphere (Wang, 2003).
Previously, it was thought that most particles in the stratosphere came from volcanoes or were generated by high-flying aircraft. Collection of air samples from the stratosphere in 2003 led to detection of carbon monoxide and other gases related to combustion at a level 30 times higher than can be accounted for by commercial aircraft.
Satellite observation of smoke plumes from wildfires revealed that the plumes could be traced intact for distances exceeding 5,000 kilometers. This observation suggests that the plumes were in the stratosphere above weather conditions that would have brought the plume back to earth.
Atmospheric models suggest that these concentrations of sooty particles could increase absorption of incoming solar radiation during winter months by as much as 15% (Baumgardner, et al., 2003).
The massive forest fire in Indonesia (1997/1998) released approx. 2.57 gigatonnes of Carbon Dioxide into the atmosphere (source: Nature magazine, November 2002). During 1997-1998, the total amount of Carbon Dioxide released to the atmosphere was 6 gigatonnes. Most of the Carbon Dioxide gas is released by the continuous underground smouldering fire on the peat bogs.
After the end of a wildfire, houses sometimes experience an ember attack - an onslaught of burning twigs or branches that can ignite a fire in the house.
Fires good and bad
Fire is sometimes essential for forest regeneration, or provides tangible benefits for local communities. In other cases it destroys forests and has dire social and economic consequences.
Forest fires are a natural part of ecosystems in many, but not all, forest types: in boreal and dry tropical forests for example they are a frequent and expected feature, while in tropical moist forests they would naturally be absent or at least rare enough to play a negligible role in ecology.
Notable wildfires
  • The Milford Flat Fire which burned in 2007 in Utah is statistically the largest fire burning in Utah's history. At the time,Governor Jon Huntsman, Jr. stated that it is the biggest fire burning in the world. This fire burned 363,052 acres.
  • The 2003 Okanagan Mountain Park Fire was started by a lightning strike near Rattlesnake Island in Okanagan Mountain Park in British Columbia, Canada, during one of the driest summers in the past decade. The final size of the firestorm was over 250 square kilometres (61,776 acres). 60 fire departments, 1,400 armed forces troops and 1,000 forest fire fighters took part in controlling the fire, but were largely helpless in stopping the disaster.
  • The Yellowstone National Park Fire of 1988 burned well over 793,880 acres (321,271 ha) before the winter snows put out the flames. (See: Yellowstone fires of 1988)
  • One of the largest known wild fires, was the Great Fire of 1910, that burned in Montana and Idaho.
  • The Zaca Fire burned Los Padres NF, CA. It burned 240,207 acres. It is the 2nd largest recorded fire in California.
  • Siege of 1987 Refers to a complex of fires in northern California and southern Oregon that burned a total of about 650,000 acres. These fires were started by a large lightning storm in late August. The storm started roughly 1600 new fires, most caused by dry lightning. Firefighting efforts continued into October, before the majority of the fires were controlled.
  • McNally Fire Sequoia NF burned roughly 151,000 acres in 2002, and is the largest wildfire recorded in the forest's history.
  • The 2003 Canberra bushfires infinged on the Australian capital itself. A firestorm raced through Canberra suburbs on January 18 2003 and damaged or destroyed 431 homes.
  • The 2007 Greek fires were some of the deadliest in world history, killing at least 64 people in Peloponnese and Evia

Source:http://encyclopedia.thefreedictionary.com/Forest+Fires

Forest fire: A Threat for conservation in Nepal

On March 12, 2009, the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Aqua satellite caught a glimpse of a relatively rare event: large–scale forest fires in the Himalaya Mountains of Nepal. Places where the sensor detected active fires are outlined in red. The numerous small fires in southern Nepal may not be wildfires, but rather agricultural or other land-management fires.
The image is centered on Nepal, and it shows the towering Himalaya Mountains arcing through the small country. Many national parks and conservation areas are located along the northern border of the country, and the fires appear to be burning in or very near some of them. Five people were killed by the forest fire southwest of Annapurna in early March; according to a news report they were overtaken while in the forest gathering firewood. According to that report, Nepal commonly experiences some small forest fires each spring, which is the end of the dry season there. However, conditions during the fall and winter of 2008 and 2009 were unusually dry, and fires set by poachers to flush game may have gotten out of control.

Tuesday, March 17, 2009

Climate Change: The Evidence

Our world is getting warmer. Over the last 100 years the average global surface temperature has risen by about 0.74C.

This seemingly small rise has already had a significant effect on our planet.

For example, the record books have had to be re-written recently, as 11 of the 12 hottest years recorded so far have all taken place since 1995.

It is "very likely" that the rising level of carbon dioxide in the atmosphere is the cause of climate change, according to the Intergovernmental Panel on Climate Change (IPCC).

Human activities, such as burning fossil fuels, are the primary source behind this increase.
Source:http://news.bbc.co.uk/2/shared/spl/hi/guides/457000/457037/html/default.stm

Himalayas and Climate Change

The Hindu-Kush-Himalayan (HKH) region in South Asia has remained a nagging gap in the global climate change knowledge bank.
In the absence of field studies and adequate data, the impact of global warming in the area stretching from Afghanistan in the west to Burma in the east is largely unknown.
In effect, there has been virtually no climate change adaptation plan for the zone, which is ecologically hypersensitive, yet a vital natural service provider.
Millions of people in the region, most of them poor ones who would be hardest hit by climate change, rely on these natural systems including river waters and forests.
But if what experts and government officials from the region and international organisations have recently agreed on is translated into action, the crippling information gap could become a matter of the past.
They have come up with a plan to first gather key information on the impacts of climate change in the region, and then chalk out responses.
"At present the lack of basic environmental data for the Himalayan region is so serious that the IPCC, the world's apex body on climate change, says that the region is a white spot for data," say officials with the International Centre for Integrated Mountain Development (ICIMOD).
ICIMOD is a Kathmandu-based international organisation that together with UNESCO recently organised a meeting for the initiative.
"The meeting discussed ways of systematically gathering and sharing the information needed, developing a reliable picture of the present situation, and formulating approaches to respond," they say.
The regional initiative is in line with UNESCO's strategy for co-ordinated research on global change in mountain biosphere reserves around the world.
Alarming signs
Seven landscapes have been identified in the HKH region for the studies, and they are transboundary areas between eight countries - with Burma the farthest east, and Kyrgyzstan at the western end.
"It will be a comprehensive study of all ecological aspects," says Eklabya Sharma, environmental programme manager with ICIMOD.
"Before, such studies have happened here and there, but this time we are adopting a transect approach, which means it will cover latitudinal (from north to south) and altitudinal (high altitude) locations.
"The idea is to encourage everyone from big global programmes to individual researchers to focus their efforts in these sites, under a co-ordinated arrangement that helps make all the information available for everyone."
Although scientists will have cryosphere issues, Ramsar sites, biodiversity hotpots and endemic species on their radars, they will be zooming in on high altitudes that are already bearing the brunt of climate change in the region.
"This is where we have found the temperature rising between 0.1C to 0.4C in a year, and that means species are shifting to higher altitudes at the rate of 80 to 200 metres in 10 years," says Mr Sharma.
"This is quite alarming."
That is one of the reasons why, immediately after the meeting, the United Nations Environment Programme (UNEP) and ICIMOD launched a study in the trans-Himalayan Kailash sacred landscape area, criss-crossing Nepal and Chinese-controlled Tibet.
The two organisations together issued a warning in 2002 that 20 glacial lakes in Nepal and 24 in Bhutan were rapidly filling up, due to global warming-induced fast glacier melting, and that they could burst anytime.
The report was based on satellite images, but there have been no follow-up studies, even though glaciologists have called for urgent further investigation.
Out of balance
There are 3,300 glaciers in the Nepalese Himalayas and 2,300 of them contain glacial lakes that are quietly growing because of rising temperatures. But a sufficiently close eye is not being kept on them, campaigners say.
Fast-melting Himalayan glaciers often find a place in climate change reports, papers and discussions.
But how fast are they melting? And with what consequences for Himalayan ecology and the enormous human population depending on it?
These are questions awaiting long overdue field studies.
"We need to get the data to fill in the gap the IPCC report has," says Gregory Greenwood, of the Mountain Research Initiative, who also participated in the meeting aimed at launching co-ordinated studies in the HKH region.
"Records of directly measured glacier mass balances are few and stretch back only to the mid-20th Century," reads one of the latest IPCC reports.
"Because of the very intensive fieldwork required, these records are biased towards logistically and morphologically 'easy' glaciers.
"An effective strategy for advancing the understanding of adverse impacts of climate change in Asia will require strengthening the academic and research institutions.
"It will be necessary to conduct innovative research on the response of human and natural systems to multiple stresses at various levels and scales," the report says.
That goal could perhaps be met to some extent if the latest bid for launching detailed field studies in the HKH region works.
Money talks
But those who have been in the climate business for years now say it is largely a money matter.
"The need for such studies is a compelling story, but true success will be getting the funding," says Mr Greenwood.
"Organisations that have been advocating such studies will have to keep beating the drum."
Then there are the ultra-sensitive geopolitical issues that have seen countries in the region not sharing information on aspects such as water resources.
But on a positive note, key regional players have of late hinted that they may co-operate in the fight against climate change.
In a recently released white paper on climate change, China has committed itself to international co-operation.
"In recent years, China's president and premier have both stated China's position on international co-operation on climate change at multilateral and bilateral exchanges, energetically promoting global action to cope with climate change," read the document.
Another major player in the region, India, has stressed a regional approach in the climate change action plan it launched earlier this year.
"That has been quite encouraging for us as most of the studies will have to be transboundary, and that will mean co-operation on the part of the countries in the region," says Mr Sharma.
If the co-operation is there and of course, the money, the HKH region will perhaps no more remain a hole in the climate change information repository.