Mostrando entradas con la etiqueta Hurricane. Mostrar todas las entradas
Mostrando entradas con la etiqueta Hurricane. Mostrar todas las entradas

domingo, 25 de agosto de 2013

NASA - NASA Invites Media to Learn About Airborne Hurricane Mission

NASA's HS3 Mission Analyzes Saharan Dust Layer Over Eastern Atlantic
Aug. 23, 2013
Global Hawk flight path
This infrared image from NOAA's GOES-East satellite on Aug. 20 shows the Global Hawk crossing the low-level remnants of Erin. Erin's low-level clouds appear as a faint circulation. The green path is the direction the Global Hawk came from. The red line represents the path the aircraft would follow.
Image Credit:
NASA/NOAA
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Global Hawk track overlaid on dust forecast (left) and temperature and dew point data graph (right)
The Global Hawk track overlaid on the GEOS-5 dust forecast (red shading). Green symbols show the locations of real-time S-HIS temperature and dew point temperature retrievals (right image, from the location of the plane symbol in the left image) which shows very dry air over the remnants of Erin.
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NASA
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Global Hawk lidar data
The Global Hawk’s Cloud Physics Lidar analyzed the Saharan Air Layer and showed an elevated dust layer (dark blue shading between 1.5 to 2.8 miles). The red shading beneath shows low-level clouds associated with Erin’s remnants. Lighter shading near 9.3 miles are thin cirrus clouds.
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NASA
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One of two of NASA's Global Hawk unmanned aircraft flew over the remnants of Tropical Storm Erin and investigated the Saharan Air Layer in the Eastern Atlantic Ocean on Aug. 20 and 21. The instruments aboard the Global Hawk sampled the environment of ex-Erin and revealed an elevated dust layer overrunning the storm.
"Our goal with this flight was to look at how the Saharan air would move around or into the former storm, but the circulation was so shallow and weak that, according to our instruments, the Saharan air simply moved westward right over what was left of Erin,"
said Scott A. Braun, HS3 principal investigator and a research meteorologist at NASA's Goddard Space Flight Center in Greenbelt, Md.
Two Global Hawks are flying as part of HS3, short for NASA's Hurricane and Severe Storm Sentinel mission, this year out of NASA’s Wallops Flight Facility at Wallops Island, Va. Global Hawk aircraft are well-suited for hurricane investigations because they can fly for as long as 28 hours and over-fly hurricanes at altitudes greater than 60,000 feet (18.3 km).
One of the purposes of the HS3 mission is to address the controversial role of the Saharan Air Layer in tropical storm formation and intensification. On its first flight out of Wallops, a Global Hawk obtained data about the SAL using several instruments aboard.
The Cloud Physics Lidar, or CPL, instrument analyzed the SAL and showed an elevated dust layer between about 1.5 and 2.8 miles (2.5 and 4.5 km) overrunning the remnants of Erin. The low-level clouds associated with what was left of Erin were located below 1.2 miles (2 km).
The CPL is an airborne lidar system designed specifically for studying clouds and aerosols. CPL will study cloud- and dust-layer boundaries and will provide optical depth or thickness of aerosols and clouds.
Another instrument aboard the Global Hawk measured temperature and dewpoint. "The scanning High-resolution Interferometer Sounder showed very dry air over the remnants of Erin," Braun said.
The Global Hawk is expected to make another trip to analyze the Saharan Air Layer on Aug. 24-25.
HS3 is a mission that brings together several NASA centers with federal and university partners to investigate the processes that underlie hurricane formation and intensity change in the Atlantic Ocean basin. Among those factors, HS3 will address the controversial role of the hot, dry and dusty Saharan Air Layer in tropical storm formation and intensification and the extent to which deep convection in the inner-core region of storms is a key driver of intensity change.
The HS3 mission will operate between Aug. 20 and Sept. 23. The Atlantic hurricane season runs from June 1 to Nov. 30 and usually peaks in early to mid-September.
Wallops is one of several NASA centers involved with the HS3 mission. The Earth Science Projects Office at NASA’s Ames Research Center in Moffett Field, Calif., manages the project. Other participants include Goddard, NASA’s Dryden Flight Research Center in Edwards, Calif., NASA’s Marshall Space Flight Center in Huntsville, Ala., and NASA’s Jet Propulsion Laboratory in Pasadena, Calif.
The HS3 mission is funded by NASA Headquarters in Washington and managed by NASA's Earth System Science Pathfinder Program at NASA's Langley Research Center in Hampton, Va., and is one of five large field campaigns operating under the Earth Venture program. The HS3 mission also involves collaborations with various partners including the National Centers for Environmental Prediction; Naval Postgraduate School; Naval Research Laboratory; the National Oceanic and Atmospheric Administration's Hurricane Research Division and Earth System Research Laboratory; Northrop Grumman Space Technology; National Center for Atmospheric Research; State University of New York at Albany; University of Maryland, Baltimore County; University of Wisconsin; and University of Utah.
Related Links
› HS3 Mission
› NASA Hurricane Research
› NASA's Wallops Flight Facility
› NASA's Airborne Science Program
› NASA's Global Hawks
Rob Gutro
NASA's Goddard Space Flight Center, Greenbelt, Md.
NASA
Guillermo Gonzalo Sánchez Achutegui
ayabaca@gmail.com
ayabaca@hotmail.com
ayabaca@yahoo.com

domingo, 4 de agosto de 2013

NASA - A NASA Infrared Baby Picture of Tropical Depression 7E

Gil (Eastern Pacific)
08.02.13 - NASA Sees Active Tropical Eastern Pacific Ocean
satellite image of Eastern Pacific storm systems
NOAA's GOES-15 satellite captured a very active Eastern Pacific ocean on Aug. 2 at 0900 UTC (5 a.m. EDT) with one hurricane and two developing tropical low pressure areas.
Image Credit:  NASA GOES Project
The Eastern Pacific Ocean has kicked into high gear on Aug. 2 and NOAA's GOES-15 satellite is watching Hurricane Gil and two developing tropical low pressure areas on both sides of Gil.
NOAA's GOES-15 satellite captured a very active Eastern Pacific ocean on Aug. 2 at 0900 UTC (5 a.m. EDT) with one hurricane and two developing tropical low pressure areas. System 91E is farthest west and approaching the Central Pacific, while Hurricane Gil and System 90E trail behind to the east. The GOES-15 infrared image was created at NASA's GOES Project at the NASA Goddard Space Flight Center, Greenbelt, Md.
System 91E Headed into Central Pacific Ocean
The low pressure area called "System 91E" has developed about 1,260 miles east-southeast of Hilo, Hawaii. The National Hurricane Center in Miami, Fla. and the Central Pacific Hurricane Center or CPHC in Honolulu, Hawaii are monitoring System 91E and expect any development to be slow. Because System 91E is moving into the Central Pacific Ocean it will soon become the responsibility of the CPHC. Currently, System 91E has a low chance of becoming a tropical cyclone during the next 48 hours.
Hurricane Gil Sandwiched
Hurricane Gil is sandwiched between two low pressure areas: System 91E to the west and System 90E to Gil's east. Gil appears to be inhibiting System 90E's development, but that may change if Gil weakens or moves farther away from the low.
At 5 p.m. EDT on Aug. 2, Gil's maximum sustained winds were near 85 mph/140 kph. The National Hurricane Center expects little change in strength during the next two days.
Gil was centered near 14.6 north latitude and 127.3 west longitude, about 1,275 miles/2,050 km west-southeast of the southern tip of Baja California, Mexico. Gil is moving west at 13 mph/20 kph and this motion is expected to continue with some decrease in forward speed during the next two days. The estimated minimum central pressure is 985 millibars.
In the GOES-15 satellite imagery Gil appears less organized and the area of strongest convection (rising air that forms the thunderstorms that make up the tropical cyclone) has been shrinking. Precipitable water imagery shows that drier air is wrapping into the eastern side of the storm and is likely the cause of the diminished organization.
Over the weekend of Aug. 3 and 4, the NHC expects slow weakening when Gil moves over progressively cooler water and into an environment of slightly stronger wind shear.
System 90E Being Affected by Hurricane Gil
Low pressure area called "System 90E" is still chasing Hurricane Gil. Located east of Gil, it is located about 900 miles southwest of the southern tip of the Baja California Peninsula of Mexico. Gil is moving westward at about 10 to 15 mph.
System 90E is producing disorganized thunderstorms, but NHC noted that if Hurricane Gil weakens, System 90E get a chance to develop. Gil's close proximity to System 90E is adversely affecting the storm's ability to organize. System 90E was given a 30 percent or medium chance of becoming a tropical cyclone over the next two days, and a higher chance over the next 5 days.
Rob Gutro
NASA's Goddard Space Flight Center, Greenbelt, Md.


08.01.13 - NASA Sees Hurricane Gil Being Chased by Developing Storm
NASA satellite captures this infrared image of Hurricane Gil on August 1 at 6:11 a.m. EDT.
The AIRS instrument aboard NASA's Aqua satellite captured this infrared image of Hurricane Gil on August 1 at 6:11 a.m. EDT. Strongest storms and heaviest rains appear around the center where cloud top temperatures exceed -63F/-52C (purple).
Image Credit:
JPL/Ed Olsen
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GOES-15 captured this image of Hurricane Gil being chased by developing low pressure System 90E on Aug 1, 2013.
NOAA's GOES-15 satellite captured this visible image of Hurricane Gil in the Eastern Pacific Ocean being chased by developing low pressure System 90E on Aug. 1 at 11 a.m. EDT.
Image Credit:
NASA GOES Project
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On July 31, NASA's TRMM satellite saw Tropical Storm Gil intensifying and the storm became a hurricane. NASA's Aqua satellite and NOAA's GOES-15 satellite captured views of Gil on Aug. 1 as it was being chased by another developing tropical system.
The Atmospheric Infrared Sounder or AIRS instrument aboard NASA's Aqua satellite captured an infrared image of Hurricane Gil on August 1 at 10:11 UTC or 6:11 a.m. EDT. Strongest storms and heaviest rains appear around the center where cloud top temperatures exceed -63F/-52.
Microwave imagery on Aug. 1 from NASA's Aqua satellite and other satellites indicated that the cloud pattern of Gil was not as organized as it appeared overnight and on July 31. Microwave imagery on Aug. 1 did not even see the ragged eye that was visible the previous day.
At 8 a.m. PDT/11 a.m. EDT on Aug. 1, Hurricane Gil's maximum sustained winds were near 80 mph (130 kph). The center of Hurricane Gil was located near latitude 14.5 north and longitude 124.2 west. Gil is far from land areas and is about 1,100 miles (1,770 km west-southwest of the southern tip of Baja California, Mexico.
Gil is moving toward the west near 13 mph/20 kph. That motion is expected to continue for the next 48 hours. The estimated minimum central pressure is 990 millibars
The National Hurricane Center noted that Gil is moving into more stable air and cooler waters, which will make any intensification over the next day brief, before the storm starts to weaken.
Traveling behind Gil, or to Gil's east, is System 90E. Imagery from NOAA's GOES-15 on Aug. 1 at 1500 UTC (11 a.m. EDT) clearly showed Hurricane Gil and System 90E trailing behind. The image was created at NASA's GOES Project at the NASA Goddard Space Flight Center in Greenbelt, Md.
This low pressure area is about 775 miles south-southwest of the southern tip of Baja California and 325 miles away from Hurricane Gil. System 90E is moving west at 10 mph and has a 50 percent chance of becoming a tropical depression in the next two days, according to the National Hurricane Center.
Rob Gutro
NASA's Goddard Space Flight Center, Greenbelt, Md.


07.31.13 - NASA Finds Powerful Storms in Quickly Intensifying Tropical Storm Gil

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NASA's TRMM satellite traveled above intensifying Tropical Storm Gil on July 31 at 12:55 a.m. EDT. The TRMM satellite pass showed that Gil was already very well organized with intense bands of rain wrapping around the center with rainfall over 5.2 inches per hour.
Image Credit:
NASA/SSAI, Hal Pierce
No sooner had Tropical Storm Flossie dissipated then another tropical cyclone called Tropical Depression 7E formed yesterday, July 30, in the eastern Pacific Ocean. NASA's TRMM satellite saw "hot towers" in the storm's center early on July 31, that indicated it would likely strengthen, and it became Tropical Storm Gil hours later.
 NASA's TRMM satellite traveled above intensifying Tropical Storm Gil on July 31 at 12:55 a.m. EDT.
NASA's TRMM satellite traveled above intensifying Tropical Storm Gil on July 31 at 12:55 a.m. EDT. The TRMM satellite pass showed that Gil was already very well organized with intense bands of rain wrapping around the center with rainfall over 5.2 inches per hour.
Image Credit:  NASA/SSAI, Hal Pierce
NASA and the Japan Space Agency's Tropical Rainfall Measuring Mission or TRMM satellite traveled above intensifying tropical storm Gil on July 31, 2013 at 0455 UTC or 12:55 a.m. EDT. The TRMM satellite pass showed that Gil was already very well organized with intense bands of rain wrapping around Gil's future eye.
TRMM's Precipitation Radar (PR) instrument found powerful storms near the center of Gil's circulation dropping rain at the rate of over 131 mm (~5.2 inches) per hour. Those powerful storms were "hot towers." A "hot tower" is a tall cumulonimbus cloud that reaches at least to the top of the troposphere, the lowest layer of the atmosphere. It extends approximately nine miles (14.5 km) high in the tropics. These towers are called "hot" because they rise to such altitude due to the large amount of latent heat. Water vapor releases this latent heat as it condenses into liquid. NASA research shows that a tropical cyclone with a hot tower in its eyewall was twice as likely to intensify within six or more hours, than a cyclone that lacked a hot tower.
On Wednesday, July 31 at 1500 UTC/11 a.m. EDT the center of Tropical Storm Gil was located near latitude 13.6 north and longitude 119.9 west, about 920 miles/1,475 km southwest of the southern tip of Baja California, Mexico. Maximum sustained winds were near 60 mph (95 kph). Gil was moving to the west-northwest at 14 mph (22 kph) and had a minimum central pressure of 1,000 millibars.
Tropical storm Gil is predicted by the National Hurricane Center or NHC to move toward the west-northwest and become a minimal hurricane with winds of 75 knots (~86 mph) by August 1.
Hal Pierce
SSAI/NASA's Goddard Space Flight Center, Greenbelt, Md.


07.30.12 - A NASA Infrared Baby Picture of Tropical Depression 7E
NASA's Aqua satellite captured this infrared image of Tropical Depression 7E on July 30 at 4:07 a.m. EDT.
The AIRS instrument aboard NASA's Aqua satellite captured this infrared image of Tropical Depression 7E on July 30 at 4:07 a.m. EDT. Strongest storms (purple) and heaviest rains are in fragmented thunderstorms around the center.
Image Credit:  NASA JPL/Ed Olsen
Tropical Depression 7E formed in the Eastern Pacific Ocean during the morning of July 30, and a NASA satellite was overhead to get an infrared baby picture. NASA's Aqua satellite passed over the depression and saw strong, but fragmented thunderstorms around the center.
The Atmospheric Infrared Sounder or AIRS instrument flies aboard NASA's Aqua satellite. AIRS creates infrared data that helps determine temperature, such as cloud top and sea surface temperatures.
AIRS captured an infrared image of Tropical Depression 7E on July 30 at 08:08 UTC/4:07 a.m. EDT. AIRS infrared data showed that the strongest storms and heaviest rains appeared in fragmented thunderstorms around the center with cloud top temperatures near -63F/-52C.
At 1500 UTC (11 a.m. EDT), newborn Tropical Depression 7E or TD7E had maximum sustained winds near 30 mph (45 kph). It was far from land and is not expected to affect any land areas as it moves farther out to sea. TD7E was centered near 12.2 north latitude and 114.9 west longitude, about 810 miles/1,300 km south-southwest of the southern tip of Baja California, Mexico. TD7E is moving to the west-northwest at 16 mph/26 kph and had a minimum central pressure of 1,008 millibars.
Forecasters at the National Hurricane Center noted in their discussion that TD7E is located in the Inter-tropical Convergence Zone or ITCZ, but has plenty of moisture and is over warm sea surface temperatures that will help it strengthen over the next couple of days.
Tropical Depression 7E is expected to move west-northwest and intensify into a tropical storm. The National Hurricane Center noted that it could later become a hurricane.
Rob Gutro
NASA's Goddard Space Flight Center, Greenbelt, Md.
NASA
Guillermo Gonzalo Sánchez Achutegui

domingo, 14 de julio de 2013

NASA : Remnants of Tropical Storm Chantal



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Remnants of Tropical Storm Chantal
In this image taken by the GOES-West satellite at 8 a.m. EDT on July 10, 2013, Chantal's satellite presentation has deteriorated markedly and is barely classifiable by the Dvorak technique, a method that uses satellite imagery to estimate the intensity of a tropical system. The 5 p.m. advisory from the National Hurricane Center on the same day indicated that Chantal had degenerated into a tropical wave.
Image Credit: NOAA/NASA GOES Project
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Guillermo Gonzalo Sánchez Achutegui
ayabaca@gmail.com
ayabaca@hotmail.com
ayabaca@yahoo.com