The fire season in 2011 is proving to be one of the most extreme in recent years. La NiƱa rains allowed thick grass to grow across Australia’s normally dry interior. The grass dried over the winter and is now an abundant source of fuel.
The fire season in 2011 is proving to be one of the most extreme in recent years. La NiƱa rains allowed thick grass to grow across Australia’s normally dry interior. The grass dried over the winter and is now an abundant source of fuel.
The images show the volcano in false-color (above) and natural-color (below) on September 28, 2011. Heat from vents in Nabro’s central crater is visible as a red glow in the false-color image. Another hotspot about 1,300 meters (4,600 feet) south of the vents reveals an active lava flow. A pale halo surrounding the vents indicates the presence of a tenuous volcanic plume. South of Nabro’s crater, the dark, nearly black areas are coated with ash so thick it completely covers the sparse vegetation. On either side of this region is a thinner layer of ash with some bright green vegetation (exaggerated in false-color) poking through.
In the natural-color image, the arid landscape is light brown where it is not covered by ash. The ash is black, while a fresh lava flow, spewed out in the last two weeks of June, is dark brown. More fresh lava flows surround the active vents. On either side of Nabro’s caldera, ephemeral streams have washed away the ash, leaving light-colored channels behind—a first sign of the erosion that will reshape, and eventually remove, what the eruption built.
On September 9, the sea ice extent was very close to the record low set in 2007, according to the National Snow and Ice Data Center (NSIDC). Scientists at the University of Bremen, who use a slightly different method to calculate sea ice extent from AMSR-E measurements, declared that 2011 surpassed 2007, setting a new record low.
On September 9, sea ice covered 4.33 million square kilometers (1.67 million square miles), NSIDC reported. The 2011 low is 2.38 million square kilometers (919,000 square miles) below the average minimum extent measured between 1979 and 2000. Late season melt or a shift in wind patterns could still decrease the sea ice extent before the winter freeze-up begins.
In 2007—the last time sea ice reached similarly low levels—conditions were ideal for melt. Skies were clear, wind patterns thinned the ice, and warm air temperatures melted the ice. Weather patterns in 2011, by contrast, were typical. This means, NSIDC scientists say, that the ice was thin and spread out before the melting even started in the summer of 2011. It is a sign that Arctic sea ice is thinning. Indeed the last five years include the five lowest sea ice extents since records began in 1979, and much of that trend has been caused by global warming, says NASA Cryosphere Program manager Tom Wagner in his video interpretation of the 2011 sea ice record (43 MB MPEG-4).
This astronaut photograph highlights the mostly dry bed of Owens Lake, located in theOwens River Valley between the Inyo Mountains and the Sierra Nevada. Shallow groundwater, springs, and seeps support minor wetlands and a central brine pool. Two bright red areas along the margins of the brine pool indicate the presence of halophilic (salt-loving) organisms known as archaeans. Gray and white materials within the lake bed are exposed sediments and salt crusts. The nearby towns of Olancha and Lone Pine are marked by the presence of green vegetation, indicating a more constant availability of water.
The present-day Owens Lake was once part of a much larger lake and river system along the northeastern border of California and Nevada during the Pleistocene Epoch (about 3 million to 12,000 years ago). Melt water from alpine glaciers in the Sierra Nevada filled the regional valleys of the Basin and Range to form glacial lakes—ancestors of the now-dry lakebeds (or playas) of Owens, Searles Lake, and China Lake.
While Searles and China Lakes dried out because of regional changes to a hotter and drier climate, Owens Lake became desiccated largely due to the diversion of the Owens River in the early 20th century to serve the needs of Los Angeles, 266 kilometers (165 miles) to the south. Following complete desiccation of the lakebed in 1926, significant amounts of windblown dust were produced. Residents of the now largely abandoned town of Keeler (on the eastern side of the lake) coined the term “Keeler fog” to describe the airborne dust.
In addition to adverse health effects on local residents, dust from Owens Lake has been linked to reductions of visibility in nearby national parks, forests, and wilderness areas. Recently, the City of Los Angeles has undertaken efforts to control dust evolution from the lakebed.
Aland vegetation is a combination of pine and deciduous forest, meadows, and farmed fields. On nearly every island, however, the region’s characteristic red rapakivi granite appears.
Modern residents of Aland cut and use the granite in buildings and pavement, but much earlier, ice sculpted these rocks. About 20,000 years ago, a massive ice sheet stretched over Scandinavia and the Gulf of Bothnia, and glacial action gradually wore the granite smooth.
The granite in this region is actually far older than the glaciers that smoothed its surface, having formed in the Proterozoic Era. The rapakivi was deposited tens of millions of years before the first amphibians crawled out of water and onto land, and hundreds of millions of years before the first dinosaurs evolved.
In the 1960s, the Soviet Union undertook a major water diversion project on the arid plains of Kazakhstan, Uzbekistan, and Turkmenistan. The region’s two major rivers, fed from snowmelt and precipitation in faraway mountains, were used to transform the desert into fields for cotton and other crops.
Although irrigation made the desert bloom, it devastated the Aral Sea. This series of images from the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Terra satellite documents the changes throughout the past decade. At the start of the series in 2000, the lake was already a fraction of its 1960 extent (black line). The Northern Aral Sea (sometimes called the Small Aral Sea) had separated from the Southern (Large) Aral Sea. The Southern Aral Sea had split into eastern and western lobes that remained tenuously connected at both ends.
By 2001, the southern connection had been severed, and the shallower eastern part retreated rapidly over the next several years. Especially large retreats in the eastern lobe of the Southern Sea appear to have occurred between 2005 and 2009, when drought limited and then cut off the flow of the Amu Darya. Water levels increased in 2010 after the drought broke and then began to dwindle again in 2011.
In a last-ditch effort to save some of the lake, Kazakhstan built a dam between the northern and southern parts of the Aral Sea. Completed in 2005, the dam was basically a death sentence for the southern Aral Sea, which was judged to be beyond saving. All of the water flowing into the desert basin from the Syr Darya now stays in the Northern Aral Sea. Between 2005 and 2006, the water levels in that part of the lake rebounded significantly and very small increases are visible throughout the rest of the time period. The differences in water color are due to changes in sediment.
Record-setting drought conditions have affected much of Texas since early 2011drying out both forest and grassland and providing ample fuel for wildfires. Relatively high winds and low humidity levels have also contributed to the rapid spread and expansion of fires. According to a report dated September 7, 2011, the Texas Forest Service had responded to 172 fires affecting an area of 546.53 square kilometers (135,051 acres) over the preceding seven days. Fires near Bastrop (to the east of Austin) had destroyed 785 homes as of September 7, 2011.
As humanity's first reusable spacecraft, the space shuttle pushed the bounds of discovery ever farther, requiring not only advanced technologies but the tremendous effort of a vast workforce. Thousands of civil servants and contractors throughout NASA's field centers and across the nation have demonstrated an unwavering commitment to mission success and the greater goal of space exploration.
Flooding in more than 1,000 villages in Bihar forced residents from their homes by late August 2011, the Indo-Asian News Service reported. After two years of drought, the Kosi River and Ganga (Ganges) Rivers were rising rapidly.
The Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Terra satellite captured these images of a stretch of the Ganga, or Ganges, River around Patna August 30, 2011 (top), and June 23, 2011 (bottom). These images use a combination of infrared and visible light to increase contrast between water and land. Water ranges in color from electric blue to navy. Vegetation is green. Clouds are pale blue-green.
Water often rises along the Ganga during monsoon season, which typically lasts from June to August. In August 2011, however, waters rose high enough to pass the danger mark in multiple locations. In the image from August, the swollen river has spilled onto floodplains to the north and south. The Indo-Asian News Service reported widespread damage to crops as well as destroyed homes.