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

viernes, 7 de octubre de 2016

NASA: Space Station Flyover of Hurricane Matthew .- Estación Espacial Internacional pasó muy elevado del huracán Mateo......

http://www.nasa.gov/image-feature/space-station-flyover-of-hurricane-matthew

Hurricane Matthew photographed from space station window with solar arrays visible in the upper right corner
The International Space Station has tracked Hurricane Matthew all week, providing images and video from low Earth orbit as the storm hit the Caribbean Sea and made its way towards Florida. In this photograph taken by Expedition 49 Flight Engineer Kate Rubins on Oct. 4, 2016, at 21:05 GMT, the hurricane's clouds extend across the frame and the space station's solar arrays are visible at the upper-right corner of the image. As the hurricane strengthens and approaches the Florida coast, NASA and NOAA satellites continue to provide forecasters and scientists valuable data on the development and changes in the storm.
Image Credit: NASA
Last Updated: Oct. 6, 2016
Editor: Sarah Loff
Tags:  Earth, Expedition 49, Hurricanes, Image of the Day, International Space Station (ISS),
NASA
Guillermo Gonzalo Sánchez Achutegui
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miércoles, 18 de noviembre de 2015

NASA : 97B - North Indian Ocean .-

Hola amigos:  A VUELO DE UN QUINDE EL BLOG., Durante la semana pasada extrema precipitaciones a partir de dos móviles áreas de baja presión tropicales lentas causado graves inundaciones en el sureste de la India. Uno de los puntos bajos, designado Sistema 97B continuaron persistir a lo largo de la costa sudeste de la India el 17 de noviembre como el sistema 97B y otra área de baja presión se redujo fuertes lluvias, la NASA y socios en todo el mundo se reunieron datos utilizando una serie de satélites.
Las inundaciones han causado tantos como 70 muertes. La ciudad de Chennai, en el estado de Tamil Nadu fueron golpeados excepcionalmente duro, como se informó de 59 personas asesinadas allí.
More information....

NASA Measures India's Deadly Flooding Rains


During the past week extreme rainfall from two slow moving tropical low pressure areas caused severe flooding in southeastern India. One of the lows, designated System 97B continued to linger along the southeastern Indian coast on November 17. As System 97B and another low pressure area dropped heavy rainfall, NASA and partners around the world gathered data using an array of satellites.

The flooding has caused as many as 70 reported deaths. The city of Chennai in the state of Tamil Nadu were hit exceptionally hard, as 59 people were reported killed there.
 
GPM image of 97B
An analysis of rainfall data from November 9 to 16, 2015 showed up to 550 mm (21.7 inches) of rain drenched India's southeastern coast in the state of Tamil Nadu. Over 200 mm (7.9 inches) fell in large areas of southeastern India and northern Sri Lanka.
Credits: NASA/JAXA/Hal Pierce

NASA's Integrated Multi-satellite Retrievals for GPM (IMERG) combines all data from 12 satellites into a global map of rainfall at half hourly intervals. The rainfall accumulation analysis above was computed from data generated by IMERG during the past week from November 9 to 16, 2015. An analysis of those data indicates that during the past week up to 550 mm (21.7 inches) of rain drenched India's southeastern coast in the state of Tamil Nadu. Rainfall totals of over 200 mm (7.9 inches) were measured in large areas of southeastern India and northern Sri Lanka.

Suomi NPP image of 97B
On Nov. 17 at 7:32 UTC (2:32 a.m. EST) the Visible Infrared Imaging Radiometer Suite (VIIRS) instrument aboard NASA-NOAA's Suomi NPP satellite captured a visible image of System 97B hugging the Indian coast.
Credits: NASA/NOAA/NRL
The Integrated Multi-satellitE Retrievals for GPM (IMERG) creates a merged precipitation product from the GPM constellation of satellites. These satellites include: DMSP (Defense Mapping Satellite Program) satellites from the U.S. Department of Defense, GCOM-W from the Japan Aerospace Exploration Agency (JAXA), Megha-Tropiques from the Centre National D’etudies Spatiales (CNES) and Indian Space Research Organization (ISRO), NOAA series from the National Oceanic and Atmospheric Administration (NOAA), Suomi-NPP from NOAA-NASA, and MetOps from the European Organisation for the Exploitation of Meteorological Satellites (EUMETSAT).  All of the instruments (radiometers) onboard the constellation partners are inter-calibrated with information from the GPM Core Observatory’s GPM Microwave Imager (GMI) and Dual-frequency Precipitation Radar (DPR). 

On November 16 at 1800 UTC (1 p.m. EST) System 97B was located just 55 nautical miles east of Chennai, India. It was centered near 13.2 degrees north latitude and 81.1 degrees east longitude. 

On Nov. 17 at 7:32 UTC (2:32 a.m. EST) the Visible Infrared Imaging Radiometer Suite (VIIRS) instrument aboard NASA-NOAA's Suomi NPP satellite captured a visible image of System 97B. The storm stretched over southwestern Bay of Bengal near and the northern coast of Tamil Nadu and southern Andhra Pradesh coast. The VIIRS image showed bands of thunderstorms wrapping from the northern quadrant into the southwestern quadrant. The Joint Typhoon Warning Center noted that computer models show that System 97B is expected to move in a northerly direction. Maximum sustained winds are estimated between 20 and 25 knots (23 to 28.7 mph/37 to 46.3 kph), and System 97B has a minimum central pressure near 1004 millibars.

The low pressure area continued to generate heavy rain in Tamil Nadu and at isolated places over south coastal Andhra Pradesh. For forecasts and updates from the Indian Meteorological Department, visit: http://www.imd.gov.in.

For more about NASA's Precipitation Measurement Missions, visit:

Harold F. Pierce / Rob Gutro
SSAI/NASA's Goddard Space Flight Center

Last Updated: Nov. 17, 2015
Editor: Lynn Jenner
Tags:  GPM (Global Precipitation Measurement), Hazards, Hurricanes, Suomi NPP (National Polar-orbiting Partnership),
NASA
Guillermo Gonzalo Sánchez Achutegui
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NASA : 27W - Northwestern Pacific Ocean .- 27W - Noroeste del Océano Pacífico

Hola amigos: A VUELO DE UN QUINDE EL BLOG., La tormenta tropical 27W fue captada en una imagen de luz visible del instrumento VIIRS bordo Suomi NPP satélite de la NASA-NOAA, el 17 de noviembre a las 0224 GMT (16 de noviembre a las 9:24 pm hora del este). La imagen VIIRS mostró el centro de bajo nivel de la circulación siguió consolidando. Bandas anchas de tormentas eléctricas en el cuadrante sur de la tormenta fueron terminando en el lado oriental de la tormenta.
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NASA Sees Tropical Storm 27W Form in Marianas Islands, Warnings Up


The tropical low pressure area previously known as System 95W consolidated and was classified as a Tropical Depression 27W on November 17, 2015. The Suomi NPP satellite captured a view of the strengthening storm as warnings were posted in Micronesia.

Suomi NPP image of 27W
The VIIRS instrument aboard NASA-NOAA's Suomi NPP satellite saw Tropical Storm 27W on Nov. 17, as wide bands of thunderstorms in the southern quadrant of the storm were wrapping into the eastern side.
Credits: NASA/NOAA/NRL
 
Tropical Storm 27W was captured in a visible-light image from the VIIRS instrument aboard NASA-NOAA's Suomi NPP satellite on Nov. 17 at 0224 UTC (Nov. 16 at 9:24 p.m. EST). The VIIRS image showed the low-level center of circulation continued to consolidate. Wide bands of thunderstorms in the southern quadrant of the storm were wrapping into the eastern side of the storm.  

At 1200 UTC (7 a.m. EST) on November 17, a tropical storm warning was in effect for Sapwuafik, Micronesia. Tropical storm force winds of 39 to 73 mph are expected within 24 hours. A tropical storm watch remains in effect for Pohnpei, Nukuoro and Pakin in Pohnpei State. These islands are part of the Federated States of Micronesia. A tropical storm watch is also in effect for Lukunor, Losap, Chuuk and Fananu in Chuuk state. A tropical storm warning means that tropical storm force winds of 39 to 73 mph are possible within 24 to 48 hours.

At 1200 UTC (7 a.m. EST) on November 17 (10 p.m. CHST (Guam) local time on Nov. 16) the center of tropical storm 27W was located by satellite near latitude 4.7 degrees north and longitude 159.8 degrees east. That's about 190 miles southeast of Pohnpei and Pakin and about 185 miles east-southeast of Sapwuafik.

27W was moving west-northwest at 18 mph. Tropical storm 27W is expected to continue on this track over the next 24 to 48 hours. Maximum sustained winds have increased to 40 mph. Tropical storm force winds extend outward up to 30 miles from the center.

The Joint Typhoon Warning Center forecast takes the tropical cyclone on a west-northwestward path passing Pohnpei, Fananu and Chuuk before intensifying to typhoon-force. The forecast calls for Tropical Cyclone 27W to be at typhoon-force as it is expected to pass just south of Guam on November 21. For local warnings and watches for Guam and the Marianas, visit NOAA's National Weather Service office in Tiyan, Guam:

Last Updated: Nov. 17, 2015
Editor: Lynn Jenner
NASA
Guillermo Gonzalo Sánchez Achutegui
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viernes, 13 de noviembre de 2015

NASA : Kate (Atlantic Ocean) .- Ciclón Kate (Océano Atlántico)

Hola amigos: A VUELO DE UN QUINDE EL BLOG., Kate se convirtió en el duodécimo llamado ciclón tropical de la temporada de huracanes del Atlántico 2015 cuando se formó cerca de el sureste de Bahamas;  el domingo 8 de noviembre de 2015. Kate volvió a curvarse hacia el noreste y se movió sin causar daños sobre las aguas abiertas del Atlántico. Intensidad de Kate alcanzó su punto máximo el 11 de noviembre 2015, con vientos de unos 65 nudos lo que es un huracán de categoría uno en la escala Saffir-Simpson de Huracanes.
More information....

Former Tropical Cyclone Kate Examined By NASA's GPM, RapidScat and NOAA's GOES-East Satellite


NASA and NOAA recently got three different views of former tropical cyclone Kate from space. The Global Precipitation Measurement mission or GPM core satellite saw heavy rainfall as Kate was transitioning into an extra-tropical cyclone on Nov. 11. The next day, NASA's RapidScat saw the system's tropical-storm force winds, and on Nov. 13, NOAA's GOES-East satellite spotted the former tropical storm in the Northern Atlantic.

GPM image of Kate
On Nov. 11, GPM found that intense storms within feeder bands there were dropping rain at a rate of over 80 mm (3.1 inches) per hour. A 3-D cross section by GPM's Radar (DPR Ku Band) through Kate's weak eye shows intense storms swirling around the northern side of the tropical cyclone.
Credits: NASA/JAXA/SSAI, Hal Pierce
 
Kate became the twelfth named tropical cyclone of the of the 2015 Atlantic hurricane season when it formed near the southeastern Bahamas on Sunday November 8, 2015. Kate re-curved toward the northeast and moved harmlessly over the open waters of the Atlantic. Kate's intensity peaked on November 11, 2015 with winds of about 65 knots making it a category one hurricane on the Saffir-Simpson Hurricane.

The GPM core observatory satellite flew above Kate on November 11, 2015 at 0926 UTC (4:26 a.m. EST) capturing data. Kate's maximum sustained winds were estimated at about 60 knots (69 mph) at that time making it a strong tropical storm. GPM's Dual-Frequency Precipitation Radar (DPR) sliced through Kate's western side and found that intense storms within feeder bands there were dropping rain at a rate of over 80 mm (3.1 inches) per hour. A 3-D cross section by GPM's Radar (DPR Ku Band) through Kate's weak eye showed intense storms swirling around the northern side of the tropical cyclone. GPM is managed by both NASA and the Japan Aerospace Exploration Agency.

Kate merged with a baroclinic zone over the north Atlantic and became an extra-tropical cyclone on November 12, 2015. A baroclinic zone is a region in which a temperature gradient exists on a constant pressure surface. Baroclinic zones are favored areas for strengthening and weakening system.

RapidScat image of Kate
On Nov. 12, RapidScat showed that strongest winds in former tropical storm Kate were in the northwestern and southeastern quadrants near 32 meters per second (71.5 mph/115.2 kph).
Credits: NASA JPL, Doug Tyler
 
On Nov. 12, the RapidScat instrument that flies aboard the International Space Station measured the surface winds associated with the low pressure area. RapidScat showed that strongest winds were in the northwestern and southeastern quadrants near 32 meters per second (71.5 mph/115.2 kph). Winds around the southwestern quadrant were weakest, while the northeastern side of the storm averaged wind speeds around 20 meters per second (44.7 mph/72 kph).

GOES-East image of Kate
On Nov. 13 at 1145 UTC (7:45 a.m. EST), the NOAA's GOES-East satellite saw the low pressure system formerly known as extra-tropical storm Kate was in the Northern Atlantic Ocean, far to the south of Greenland.
Credits: NASA/NOAA GOES Project
 
On Nov. 13 at 1145 UTC (7:45 a.m. EST), the NOAA's GOES-East satellite saw the low pressure system formerly known as extra-tropical storm Kate was in the Northern Atlantic Ocean, far to the south of Greenland. An image of the storm was created by the NASA/NOAA GOES Project at NASA's Goddard Space Flight Center in Greenbelt, Maryland. The image showed the low pressure center near 41 degrees north latitude and 47 degrees west longitude, and clouds associated with the cold front stretched south and west of the center toward the Bahamas. The low pressure center and associated cold front continued tracking to the east, across the Atlantic.

Harold F. Pierce / Rob Gutro
SSAI/NASA's Goddard Space Flight Center

Nov. 12, 2015 - NASA Spies Extra-tropical Storm Kate Racing Through North Atlantic


On November 12 at 4 a.m. EST the National Hurricane Center issued the last advisory on Extra-Tropical Cyclone Kate, located several hundred miles south-southeast of Cape Race, Newfoundland. NOAA's GOES-East satellite captured a visible light image of the storm.

GOES-West image of Kate
This NOAA GOES-West satellite visible image extra-tropical storm Kate shows the storm over 400 miles southeast of Newfoundland, Canada.
Credits: NASA/NOAA GOES Project

A NOAA GOES-West satellite visible image extra-tropical storm Kate on Nov. 12 at 1445 UTC (9:45 a.m. EST) showed the storm over 400 miles southeast of Newfoundland, Canada. Most of the clouds associated with the post-tropical storm were north and east of the center. Forecaster Beven of the National Hurricane Center said, "Satellite imagery indicates that Kate has merged with a baroclinic zone over the north Atlantic and is now an extratropical cyclone."

Kate Reached Hurricane Strength

On Nov. 10, the RapidScat instrument that flies aboard the International Space Station saw Hurricane Kate north of the Bahamas and its strongest winds were north of the center. Maximum sustained winds in both areas were as strong as 30 meters per second (67 mph/108 kph). On Nov. 11, those winds increased to hurricane force. Hurricane force winds extended outward up to 35 miles (55 km) from the center and tropical storm force winds extend outward up to 205 miles (335 km).

At 10 a.m. EST (1500 UTC) on Nov. 11 the center of Hurricane Kate was located near latitude 36.8 North, longitude 60.5 West. That put Kate's center about 395 miles (635 km) northeast of Bermuda and about 780 miles (1,260 km) south-southwest of Cape Race Newfoundland.

An Infrared Look at Kate

On Nov. 12 at 05:17 UTC (12:17 a.m. EST) infrared imagery from the Atmospheric Infrared Sounder or AIRS instrument aboard NASA's Aqua satellite showed fragmented strong storms east and north of Kate's center where cold cloud top temperatures were near -63F/-53C. Storms with cloud tops that cold (and high in the troposphere) have been shown to generate heavy rain.

Aqua satellite showed fragmented strong storms east and north of Kate's center.
On Nov. 12 at 05:17 UTC (12:17 a.m. EST) infrared imagery from the AIRS instrument aboard NASA's Aqua satellite showed fragmented strong storms east and north of Kate's center where cold cloud top temperatures were near -63F/-53C (purple).
Credits: NASA JPL, Ed Olsen
Kate Weakens and Becomes Extra-Tropical

At 4 a.m. EST on Nov. 12, Kate was classified as an extra-tropical storm. That means that a tropical cyclone has lost its "tropical" characteristics. The National Hurricane Center defines "extra-tropical" as a transition that implies both poleward displacement (meaning it moves toward the north or south pole) of the cyclone and the conversion of the cyclone's primary energy source from the release of latent heat of condensation to baroclinic (the temperature contrast between warm and cold air masses) processes. It is important to note that cyclones can become extratropical and still retain winds of hurricane or tropical storm force.

At 4 a.m. EST on Nov. 12, Kate's maximum sustained winds were near 60 knots (70 mph). Kate was centered near 40.7 degrees north latitude and 50.8 degrees west longitude, about 430 miles south-southeast of Cape Race, Newfoundland, Canada. Kate was moving to the east-northeast at 23 knots (26 mph). Minimum central pressure was 983 millibars. The post-tropical cyclone is expected to accelerate toward the east-northeast and northeast.

Kate's Fate

The National Hurricane Center expects extra-tropical storm Kate to continue weakening, but slowly over the next couple of days. The NHC forecast keeps maximum sustained winds near 45 knots (50 mph) through Nov. 15 and by Nov. 16, Kate is expected to become absorbed by an extra-tropical low pressure area.

Additional information on this system can be found in High Seas Forecasts issued by the National Weather Service at


Nov. 10, 2015 - NASA Spots Kate Speeding Away from the Bahamas


NASA-NOAA's Suomi NPP satellite and NOAA's GOES-East satellite both saw strong thunderstorms circling Tropical Storm Kate's center of circulation as the storm sped away from the Bahamas.

GOES image of Kate
This visible image Tropical Storm Kate near Bermuda was taken from NOAA's GOES-East satellite at 1430 UTC (9:30 a.m. EDT).
Credits: NASA/NOAA GOES Project

A visible image Tropical Storm Kate near Bermuda was taken from NOAA's GOES-East satellite at 1430 UTC (9:30 a.m. EDT). The GOES-East image showed the concentration of thunderstorms around the center, which is covered by a small central dense overcast, and a fragmented band of thunderstorms northeast of the center. 

When NASA-NOAA's Suomi NPP satellite passed over Kate at 7:00 UTC (2 a.m. EST) the Visible Infrared Imaging Radiometer Suite or VIIRS instrument that flies aboard looked at the storm in infrared light. Cloud top temperatures of thunderstorms around the eyewall were between minus 70 and minus 80 degrees Celsius/minus 94 and minus 112 degrees Fahrenheit.

Suomi NPP image of Kate
When NASA-NOAA's Suomi NPP satellite passed over Kate at 7:00 UTC (2 a.m. EST) the VIIRS instrument that flies aboard Suomi NPP looked at the storm in infrared light. Cloud top temperatures of thunderstorms around the eyewall were between -70 and -80 Celsius/ -94 and -112 Fahrenheit (red).
Credits: NASA/NOAA/NRL

The higher the cloud tops, the colder they are as temperatures get colder with altitude in the troposphere. Storms with cloud top temperatures that cold have the capability of generating heavy rainfall.


At 10 a.m. EST (1500 UTC) on Nov. 10, the center of Tropical Storm Kate was located near latitude 30.2 North, longitude 74.7 West. That's about 350 miles (560 km) south of Cape Hatteras, North Carolina and 600 miles (970 km) west of Bermuda.

Kate was moving toward the northeast near 21 mph (33 kph), and the National Hurricane Center expects that general motion is expected to continue today with an increase in forward speed.  On the forecast track, the center of Kate is expected to remain well offshore of the U.S. East Coast and pass north of Bermuda tonight and early Wednesday, November 11. Data from an Air Force Reserve Hurricane Hunter aircraft indicated that maximum sustained winds have increased to near 70 mph (110 kph) and Kate is forecast to become a hurricane at night on November 10. The latest minimum central pressure based on data from the aircraft is 999 millibars.

NHC forecasts Kate to turn northeastward and east-northeastward and accelerate more through Wednesday as it becomes embedded in the mid-latitude westerlies and speed into the North Atlantic. For forecast updates, visit the NHC website:

 

Nov. 09, 2015 - NASA Sees Tropical Storm Kate Form, Bahamas Under Warning


NASA's Terra satellite saw the Atlantic Ocean's twelfth tropical depression as it was forming, and an animation of NOAA's GOES-East satellite data showed its development into Tropical Storm Kate near the Bahamas.
 
This 43 second animation of infrared and visible imagery from NOAA's GOES-East satellite from Nov. 7 to 9 shows the development and movement of Tropical Storm Kate to the Bahamas.
Credits: NASA/NOAA GOES Project
 
On November 9, 2015 a Tropical Storm Warning was in effect for the central and northwestern Bahamas.

On Nov. 8, 2015 the Moderate Resolution Imaging Spectroradiometer or MODIS instrument aboard NASA's Terra satellite captured a visible image of newborn Tropical Depression 12 in the western Atlantic. Kate formed as a tropical depression at 10 p.m. EST on Nov. 8 about 115 miles (190 km) southeast of San Salvador.

MODIS image of Kate
On Nov. 8, 2015 the MODIS instrument aboard NASA's Terra satellite captured this image of newborn Tropical Depression 12 in the western Atlantic.
Credits: NASA Goddard MODIS Rapid Response Team

At 8:20 a.m. EST, Air Force Reserve hurricane hunter aircraft data indicated that Tropical Depression Twelve has strengthened to Tropical Storm Kate. The maximum sustained winds at that time were estimated to be 40 mph (65 kph) with higher gusts.

A 43 second animation of infrared and visible imagery from NOAA's GOES-East satellite over the period of satellite from Nov. 7 to 9 shows the development and movement of Tropical Storm Kate to the Bahamas. The animation was created by the NASA/NOAA GOES Project at NASA Goddard.

At 10 a.m. EST (1500 UTC) on November 9, 2015 the center of Tropical Storm Kate was located near latitude 24.5 North, longitude 75.3 West. That's just 15 miles (25 km) east-northeast of Cat Island an about 170 miles (275 km) southeast of Great Abaco Island.

Kate was moving toward the northwest near 15 mph (24 kph). The National Hurricane Center (NHC) expects Kate to turn toward the north, followed by a turn toward the north-northeast on Tuesday, November 10. Maximum sustained winds had increased to near 45 mph (75 kph) and additional strengthening is forecast during the next two days. The estimated minimum central pressure based on data from an Air Force Reserve reconnaissance aircraft is 1008 millibars.

Because the central and northwestern Bahamas are under a tropical storm warning, the National Hurricane Center said total rain accumulations of 1 to 3 inches over the Bahamas through tonight, November 3.

For updates on the forecast track of Kate, please visit the NHC website: www.nhc.noaa.gov.

Rob Gutro
NASA's Goddard Space Flight Center
Last Updated: Nov. 13, 2015
Editor: Lynn Jenner
 
NASA
Guillermo Gonzalo Sánchez Achutegui
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domingo, 1 de noviembre de 2015

NASA : Colors After the Storms .- Colores después de las tormentas

Hola amigos: A VUELO DE UN QUINDE EL BLOG., Las fuertes lluvias perjudiciales cayeron en Carolina del Sur, en el sureste de Estados Unidos a principios de octubre de 2015. Gran parte de esa agua tenía, a mediados de octubre, fluyeron en el Océano Atlántico trayendo consigo pesadas cargas de sedimentos, nutrientes y materia orgánica disuelta. La imagen de arriba, desde el Visible Infrared Imaging Radiometer Suite (VIIRS) instrumento en el satélite Suomi NPP de la NASA-NOAA, muestra la segunda vuelta, ya que interactúa con las corrientes oceánicas en 15 de octubre

Suomi NPP, lanzado el 28 de octubre de 2011, representa un primer paso fundamental en la construcción del sistema de la Tierra por satélite de observación de la próxima generación que recogerá datos sobre el cambio climático a largo plazo y las condiciones meteorológicas a corto plazo. Suomi NPP lanzado con cinco instrumentos clave, incluyendo VIIRS, un radiómetro de exploración que recoge imágenes visibles e infrarrojas y las mediciones radiométricas de la tierra, la atmósfera, la criosfera y océanos. Datos VIIRS se utiliza para medir las nubes y aerosoles propiedades, color del océano, del mar y de la temperatura de la superficie terrestre, movimiento del hielo y de la temperatura, los incendios y el albedo de la Tierra. Los climatólogos utilizan datos VIIRS para mejorar nuestra comprensión del cambio climático global.
More information............

Color image of southeast United States from satellite showing sediment runoff in ocean
Damaging heavy rains fell on South Carolina in the southeastern United States at the beginning of October 2015. Much of that water had, by mid-October, flowed into the Atlantic Ocean bringing with it heavy loads of sediment, nutrients, and dissolved organic material. The above image, from the Visible Infrared Imaging Radiometer Suite (VIIRS) instrument on NASA-NOAA's Suomi NPP satellite, shows the runoff as it interacts with ocean currents on Oct. 15.
 
Suomi NPP, launched on Oct. 28, 2011, represents a critical first step in building the next-generation Earth-observing satellite system that will collect data on long-term climate change and short-term weather conditions. Suomi NPP launched with five key instruments, including VIIRS, a scanning radiometer which collects visible and infrared imagery and radiometric measurements of the land, atmosphere, cryosphere, and oceans. VIIRS data is used to measure cloud and aerosol properties, ocean color, sea and land surface temperature, ice motion and temperature, fires, and Earth's albedo. Climatologists use VIIRS data to improve our understanding of global climate change.
Image Credit: NASA/Goddard/SuomiNPP/VIIRS via NASA's OceanColor
Last Updated: Oct. 28, 2015
Editor: Sarah Loff
NASA
Guillermo Gonzalo Sánchez Achutegui
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domingo, 15 de febrero de 2015

nsf.gov National Science Foundation - Monster hurricanes struck U.S. Northeast during prehistoric periods of ocean warming.- Huracanes monstruosos golpearon noreste de Estados Unidos durante los períodos prehistóricos de calentamiento de los océanos

Hola amigos: A VUELO DE UN QUINDE EL BLOG., la Fundación Nacional de Ciencias de Los Estados Unidos, nos informan que huracanes gigantescos o monstruosos golpearon el Nor Este de los EE,UU.: The National Science Foundation (NSF). Huracanes intensos posiblemente más poderoso que cualquier tormenta de Nueva Inglaterra ha experimentado en la historia escrita con frecuencia golpean la región durante el primer milenio, desde el pico del Imperio Romano hasta la altura de la Edad Media, según los resultados de un nuevo estudio.
El hallazgo podría tener implicaciones para la comprensión de la intensidad y frecuencia de los huracanes los EE.UU. Noreste puede experimentar en el futuro.
 
More infomation.....

Scientists find clues in sediment deposits on Cape Cod

Waves crashed ashore in Woods Hole, Mass., during a 1938 hurricane.
Waves crashed ashore in Woods Hole, Mass., during a 1938 hurricane.
Credit and Larger Version
February 11, 2015
Intense hurricanes possibly more powerful than any storms New England has experienced in recorded history frequently pounded the region during the first millennium, from the peak of the Roman Empire to the height of the Middle Ages, according to results of a new study.
The finding could have implications for understanding the intensity and frequency of hurricanes the U.S. Northeast may experience in the future.
 
Looking back to see into the future
 
A record of sediment deposits from Cape Cod, Mass., shows evidence that 23 severe hurricanes hit New England between the years 250 and 1150, the equivalent of a severe storm about once every 40 years on average.
Many of these hurricanes were likely more intense than any that have hit the area in recorded history.
"The ability to produce and synthesize thousands of years of data on hurricane paths and frequencies is revolutionizing our understanding of what controls where and how often these dangerous storms make landfall," said Candace Major, program director in the National Science Foundation's Division of Ocean Sciences, which funded the research.
The prehistoric hurricanes were likely category 3 storms (such as Hurricane Katrina) or category 4 storms (Hurricane Hugo) that would be catastrophic if they hit the region today, according to Jeff Donnelly, a scientist at the Woods Hole Oceanographic Institution in Massachusetts, and lead author of a paper on the results published online today in Earth's Future, a journal of the American Geophysical Union.
 
Hurricane record extended by centuries
 
The study is the first to find evidence of historically unprecedented hurricane activity along the northern East Coast of the United States.
It also extends the hurricane record for the region by hundreds of years, back to the first century.
"These records suggest that the pre-historical interval was unlike what we've seen in the last few hundred years," said Donnelly.
The most powerful storm to hit Cape Cod in recent times was Hurricane Bob in 1991, a category 2 storm that was one of the costliest in New England history.
Storms of that intensity have only reached the region three times since the 1600s, according to Donnelly.
 
Warmer sea surface temperaturas
 
The intense prehistoric hurricanes were fueled in part by warmer sea surface temperatures in the Atlantic Ocean than have been the norm off the U.S. East Coast over the last few hundred years.
However, as ocean temperatures have slowly inched upward in recent decades, tropical North Atlantic sea surface temperatures have surpassed the warmth of prehistoric levels--and are expected to warm more over the next century as the climate heats up, Donnelly said.
"We hope this study broadens our sense of what is possible and what we should expect in a warmer climate," Donnelly said. "We may need to begin planning for a category 3 hurricane landfall every decade or so rather than every 100 or 200 years.
"The risk may be much greater than we anticipated."
 
Buried in sediment: hurricane remains
 
Donnelly and colleagues examined sediment deposits from Salt Pond near Falmouth on Cape Cod. The pond is separated from the ocean by a 1.3- to 1.8-meter (4.3 to 5.9-foot) high sand barrier.
Over hundreds of years, strong hurricanes have deposited sediment over the barrier and into the pond where it has remained undisturbed.
The researchers extracted nine-meter (30-foot) deep sediment cores, which they then analyzed in a laboratory.
Similar to reading a tree ring to tell the age of a tree and the climate conditions that existed in a given year, scientists can read a sediment core to determine when intense hurricanes occurred.
The paper's authors found evidence of 32 prehistoric hurricanes, along with the remains of three documented storms that occurred in 1991, 1675 and 1635.
The sediments showed that there were two periods of intense hurricane activity on Cape Cod -- from 150 to 1150, and 1400 to 1675.
The earlier period of powerful hurricane activity matched previous studies that found evidence of hurricanes during the same period in more southerly areas of the western North Atlantic Ocean basin--from the Caribbean to the Gulf Coast.
 
Powerful storms also battered more southerly U.S. coasts
 
The new study suggests that these powerful southern storms also battered the coast farther north through New England from 250 to 1150.
These early storms were more frequent, and in some cases were likely more intense, than the most severe hurricanes Cape Cod has seen in historical times, including Hurricane Bob in 1991 and a 1635 hurricane that generated a 20-foot storm surge, according to Donnelly.
The hurricane activity continued in the Caribbean and Gulf of Mexico until 1400, although there was a lull during this time in New England.
A shift in hurricane activity in the North Atlantic occurred around 1400, when activity picked up from the Bahamas to New England, until about 1675.
Co-authors of the paper are: Andrea Hawkes of the University of North Carolina Wilmington; Philip Lane (deceased); Dana MacDonald, University of Massachusetts, Amherst; Bryan Shuman, University of Wyoming; Michael Toomey, The University of Texas at Austin; Peter van Hengstum, Texas A&M University at Galveston; and Jonathan Woodruff, University of Massachusetts, Amherst.
-NSF-
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Related WebsitesNSF Grant: Tracking Sea-level Source Contributions: A Hemispheric Approach to High Resolution Sea-level Variation Over the Last Two Millennia:


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Scientists in a boat collecting a sediment core
Scientists collect a sediment core; the sediment shows intense storms going back 2,000 years.
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Sediment core section
Sediment core section; light-colored sand at 22.7 feet down is evidence of an intense past storm.
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Home in Union Beach, N.J., destroyed by a Hurricane Sandy storm tide in 2012.
Home in Union Beach, N.J., destroyed by a Hurricane Sandy storm tide in 2012.
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Satellite view of Hurricane Earl as it threatens the U.S. East Coast in 2010.
Satellite view of Hurricane Earl as it threatens the U.S. East Coast in 2010.
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Aerial image  showing houses and flooded land on Dauphin Island, Ala.,
Aerial image of Dauphin Island, Ala., following Hurricane Katrina in 2005.
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The National Science Foundation (NSF)
Guillermo Gonzalo Sánchez Achutegui
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