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

jueves, 6 de febrero de 2014

This Bionic Hand Allows Amputee to 'Feel' Again

Image credit: alexpb

It seems like every other day we read about some far-out, new technology that makes us scratch our heads and say, "What the heck?" In this series, we'll take a look at all types of crazy new gadgets, apps and other technologies -- and the entrepreneurs dreaming them up.

One thing's for sure: no "bionic man" has ever been able to do this before.

In 2004, Dennis Aabo Sørensen lost his left hand after a firework exploded during a New Year's Eve celebration.

Little did he know that, in order to 'feel' again, all he had to do was wait for prosthetic technology to advance to the stage where electrodes could be surgically implanted in his nerves and connected to a bionic hand.

Nine years later, that day has arrived.

With the help of a high profile team of international robotic experts, Sørensen received said bionic hand, which allowed him to tell the shape and stiffness of objects while blindfolded.

Scientists have been working on the project of touch sensitive prosthetics for years now, but this is said to be the first time that an amputee has experienced real-time touch sensations through a bionic hand. Silvestro Micera -- a researcher who has worked on the project for the past 15 years -- and his team added sensors to the artificial hand, which could detect and measure information about touch, the BBC reported. Using computer algorithms, the researchers converted the electrical signals they emitted into an impulse that sensory nerves could read.

Sørensen, for his part, was in complete awe: "Suddenly you could see my left hand was talking to my brain again and it was magic," he told USA Today, when asked to describe the first moment he could 'feel' again after nine years. "It was surreal. I grabbed the object in my hand and knew it was round. It was a baseball."



Unfortunately, due to safety restrictions (the bionic hand is still a prototype) the sensors were removed from Sørensen's hand after the experiment was completed. But the project's success points to amazing capabilities for prosthetics devices of the future: one day, scientists predict, bionic hands will not only be able to feel, but also detect texture and temperature.

Imagine the ability to feel a previously missing hand closing around an object. And sensory capable bionic arms could also allow amputees to grab things in the dark, as well as perform more nuanced tasks like cracking an egg.

While it could be up to 10 years before sensory-enabled bionic hands like Sørensen's are commercially available, the bionic future looks bright: "These results show the possibilities for amputees," Micera told USA Today, before predicting that the same technology could also be used for prosthetic legs.


ORIGINAL: Entrepreneur
February 6, 2014

miércoles, 11 de diciembre de 2013

Climate slowdown: The world won't stop warming


Warming has not peaked. Instead, it looks as if the sea is taking the strain (Image: Sesse Lind/Link Image/Gallerystock)
Editorial: "Is it time to stop worrying about global warming?"
"Global warming on pause". "Why has global warming stalled?" "Has global warming stopped?"
IF YOU have been reading the papers of late, you may be under the impression that global warming isn't proceeding as expected.

While most mainstream media have been careful to point out that the apparent lack of recent warming is probably just a temporary hiatus, a few outlets have suggested there is more to it than that. "The climate may be heating up less in response to greenhouse-gas emissions than was once thought," one magazine claimed.

What is going on? Has global warming really slowed or stopped in recent years? If so, why? And does this mean the world won't warm as ...

To continue reading this article, subscribe to receive access to all of newscientist.com, including 20 years of archive content.

What is Argo?
Argo is a global array of 3,000 free-drifting profiling floats that measures the temperature and salinity of the upper 2000 m of the ocean. This allows, for the first time, continuous monitoring of thetemperature, salinity, and velocity of the upper ocean, with all databeing relayed and made publicly available within hours aftercollection.

Positions of the floats that have delivered data within the last 30 days (AIC, updated daily):
 

Why do we need Argo?
We are increasingly concerned about global change and its regional impacts. Sea level is rising at an accelerating rate of 3 mm/year, Arctic sea ice cover is shrinking and high latitude areas are warming rapidly. Extreme weather events cause loss of life and enormous burdens on the insurance industry. Globally, 8 of the 10 warmest years since 1860, when instrumental records began, were in the past decade.

These effects are caused by a mixture of long-term climate change and natural variability. Their impacts are in some cases beneficial (lengthened growing seasons, opening of Arctic shipping routes) and in others adverse (increased coastal flooding, severe droughts, more extreme and frequent heat waves and weather events such as severe tropical cyclones).

Understanding (and eventually predicting) changes in both the atmosphere and ocean are needed to guide international actions, to optimize governments' policies and to shape industrial strategies. To make those predictions we need improved models of climate and of the entire earth system (including socio-economic factors).

Lack of sustained observations of the atmosphere, oceans and land have hindered the development and validation of climate models. An example comes from a recent analysis which concluded that the currents transporting heat northwards in the Atlantic and influencing western European climate had weakened by 30% in the past decade. This result had to be based on just five research measurements spread over 40 years. Was this change part of a trend that might lead to a major change in the Atlantic circulation, or due to natural variability that will reverse in the future, or is it an artifact of the limited observations?

In 1999, to combat this lack of data, an innovative step was taken by scientists to greatly improve the collection of observations inside the ocean through increased sampling of old and new quantities and increased coverage in terms of time and area.

That step was Argo.

Where is Argo now?
Argo deployments began in 2000 and by November 2007 the array is 100% complete. Today's tally offloats is shown in the figure above. While the Argo array is currently complete at 3000 floats, to be maintained at that level, national commitments need to provide about 800 floats per year. Additionally, Argo continues to work toward global ocean coverage. Frequently, even with the 3000 float target achieved, more floats are needed because some areas of the ocean are over populated while others have gaps that need to be filled with additional floats.

Besides float deployment, Argo has workedhard to develop two separate data streams: real time and delayed mode. A real time data delivery and qualitycontrol system has been established that delivers 90% of profiles to users via two global data centers within 24 hours. A delayed mode quality control system (DMQC) has been established and 60% of all eligible profiles have had DMQC applied.

Float reliability has improved each year and the float lifetime has been extended. Argo has developed a large user community in universities, government labs and meteorological/climateanalysis/forecasting centers. The need for global Argo observations will continue indefinitely into the future, though the technologies and design of the array will evolve as better instruments are built, models are improved, and more is learned about ocean variability.

Who Collaborates with Argo?
Argo is a major contributor to the WCRP's Climate Variability and Predictability Experiment (CLIVAR) project and tothe Global Ocean Data Assimilation Experiment (GODAE). The Argo array is part of the Global Climate Observing System/Global Ocean Observing System GCOS/GOOS).

Current Status of Argo
The broad-scale global array of temperature/salinity profiling floats, known as Argo, has already grown to be a major component of the ocean observing system. Argo is a standard to which other developing ocean observing systems can look to. For example, Argo offers ideas on various topics such as how to collaborate internationally, how to develop a data management system and how to change the way scientists think about collecting data. Deployments began in 2000 and continue today at the rate of about 800 per year


The latest picture of the Argo array.
Brief History of Argo 
The name Argo was chosen to emphasize the strong complementary relationship of the global float array with the Jason satellite altimeter mission. In Greek mythology Jason sailed in a ship called "Argo" to capture the golden fleece.
An Argo float being deployed from a research ship.
Together the Argo and Jason data sets will be assimilated into computer models developed by project GODAE (Global Ocean Data Assimilation Experiment) that will allow a test of our ability to forecast ocean climate. For the first time, the physical state of the upper ocean is being systematically measured and the data assimilated in near real-time into computer models. Argo builds on other upper-ocean ocean observing networks, extending their coverage in space an time, their depth range and accuracy, and enhancing them through the addition of salinity and velocity measurements. Argo is not confined to major shipping routes which can vary with season as the other upper-ocean observing networks are. Instead, the global array of 3,000 floats will be distributed roughly every 3 degrees (300km).

Argo's Objectives

It will provide a quantitative description of the changing state of the upper ocean and the patterns of ocean climate variability from months to decades, including heat and freshwater storage and transport.

The data will enhance the value of the Jason altimeter through measurement of subsurface temperature, salinity, and velocity, with sufficient coverage and resolution to permit interpretation of altimetric sea surface height variability.

Argo data will be used for initializing ocean and coupled ocean-atmosphere forecast models, for data assimilation and for model testing.

A primary focus of Argo is to document seasonal to decadal climate variability and to aid our understanding of its predictability. A wide range of applications for high-quality global ocean analyses is anticipated.
An Argo profile from the subtropical North Pacific
(20.25N 121.4W, May 15 2004).
This shows interleaving in the salinity data.
Argo Design and Data 
The design of the Argo network is based on experience from the present observing system, on recent knowledge of variability from the TOPEX/Poseidon altimeter, and on the requirements for climate and high-resolution ocean models.

The final array of 3000 floats will provide 100,000 temperature/salinity (T/S) profiles and velocity measurements per year distributed over the global oceans at an average 3-degree spacing. Floats will cycle to 2000m depth devery 10 days, with 4-5 year lifetimes for individual instruments. All data collected by Argo floats are publically available in near real-time via the Global Data Assembly Centers (GDACs) in Brest, France and Monterey, California after an automated quality control (QC), and in scientifically quality controlled form, delayed mode data, via the GDACs within six months of collection.  Argo Data and How to Get It

argo.avi is a float animation that explains the purpose and method of Argo. 

ORIGINAL: ARGO - UCSD
by Michael Le Page
05 December 2013 
Magazine issue 2946. Subscribe and save
For similar stories, visit the Climate Change Topic Guide

martes, 24 de julio de 2012

Soil temperature, environmental and methodological effects determine Soil CO2 efflux in Central Amazonia

ORIGINAL: SCIELO

A group of researchers from the Universidade Federal do Amazonas-UFAM, Free University-VU, Wageningen University-WUR, Instituto Nacional de Pesquisas da Amazonia-INPA and Max Planck institute-MPI, measured the soil CO2 respiration in the Central Amazon forest to understand the environmental and methodological effects on the soil CO2 emission.

The authors found that the main factor influencing the soil respiration was soil temperature, because the soil respiration followed the same pattern, while rainfall only caused a brief disturbance in soil respiration. Rainfall seems to contribute by creating favorable conditions for a quick decrease in temperature and consequently respiration followed the physical effect of soil water percolation. The methodology of automatic soil respiration used in this paper showed a better estimative of total CO2 emission in the Central Amazonian ecosystem. The authors also noticed that it was difficult to account for the rainfall effects in the simple model estimation.

According to the authors, for a better estimative of soil CO2 emissions, or to model a region and vegetation type, it is necessary to find the main influencing factors to decrease the uncertainties about the final carbon release measurements. The automated soil respiration datasets and the right procedure are a good tool to improve the technique and increase the reliability of measurements to allow a better understanding of all possible factors driven by soil respiration processes.

The study was carried out in the Cuieiras and Campina reserves near to Manaus city, during 2006 to 2008 at seven different rainforest types, four at different forests in the Cuieira reserve (plateau, slope, campinarana and valley forest) and another tree at different forests in the Campina reserve (bare soil, stunted and tall heath forest). The researchers used an automatic soil respiration system.. The authors investigated the effects of the method of ring insertion in the soil as well as of rainfall and spatial distribution on CO2 emission.

The article is published in the Acta Amazonica Journal (Vol. 42, n.2).

Contact: 
Fabrício Berton Zanchi 
Universidade Federal do Amazonas-UFAM/IEAA 

domingo, 10 de junio de 2012

CU-Boulder-led team finds microbes in extreme environment on South American volcanoes

ORIGINAL: esciencenews
June 9, 2012

A team led by the University of Colorado Boulder looking for organisms that eke out a living in some of the most inhospitable soils on Earth has found a hardy few. A new DNA analysis of rocky soils in the Martian-like landscape on some volcanoes in South America has revealed a handful of bacteria, fungi and other rudimentary organisms called archaea, which seem to have a different way of converting energy than their cousins elsewhere in the world.

"We haven't formally identified or characterized the species," said Ryan Lynch, a CU-Boulder doctoral student involved in the study. "But these are very different than anything else that has been cultured. Genetically, they're at least 5 percent different than anything else in the DNA database of 2.5 million sequences."

Life gets little encouragement on the incredibly dry slopes of the tallest volcanoes in the Atacama region, where CU-Boulder Professor Steve Schmidt and his team collected soil samples. Much of the sparse snow that falls on the terrain sublimates back to the atmosphere soon after it hits the ground, and the soil is so depleted of nutrients that nitrogen levels in the scientists' samples were below detection limits.

Ultraviolet radiation in the high-altitude environment can be twice as intense as in a low-elevation desert, said Schmidt of CU-Boulder's ecology and evolutionary biology department. While the researchers were on site, temperatures dropped to 14 degrees Fahrenheit (-15°C) one night and spiked to 133 F (56°C) the next day.

How the newfound organisms survive under such circumstances remains a mystery. Although Ryan, Schmidt and their colleagues looked for genes known to be involved in photosynthesis and peered into the cells using fluorescent techniques to look for chlorophyll, they couldn't find evidence that the microbes were photosynthetic.

Instead, they think the microbes might slowly generate energy by means of chemical reactions that extract energy and carbon from wisps of gases such as carbon monoxide and dimethylsulfide that blow into the desolate mountain area. The process wouldn't give the bugs a high-energy yield, Lynch said, but it could be enough as it adds up over time. A paper on the findings has been accepted by the Journal of Geophysical Research-Biogeosciences, published by the American Geophysical Union.

While normal soil has thousands of microbial species in just a gram of soil, and garden soils even more, remarkably few species have made their home in the barren Atacama mountain soil, the new research suggests. "To find a community dominated by less than 20 species is pretty amazing for a soil microbiologist," Schmidt said.

He has studied sites in the Peruvian Andes where, four years after a glacier retreats, there are thriving, diverse microbe communities. But on these volcanoes on the Chile-Argentina border, which rise to altitudes of more than 19,685 feet and which have been ice-free for 48,000 years, the bacterial and fungal ecosystems have not undergone succession to more diverse communities. "It's mostly due to the lack of water, we think," he said. "Without water, you're not going to develop a complex community."

"Overall, there was a good bit lower diversity in the Atacama samples than you would find in most soils, including other mountainous mineral soils," Lynch said. That makes the Atacama microbes very unusual, he added. They probably had to adapt to the extremely harsh environment, or may have evolved in different directions than similar organisms elsewhere due to long-term geographic isolation.

Growth on the mountain might be intermittent, Schmidt suggested, especially if soils only have water for a short time after snowfall. In those situations, there could be microbes that grow when it snows, then fall dormant, perhaps for years, before they grow again. High-elevation sites are great places to study simple microbial communities, ecosystems that haven't evolved past the very basics of a few bacteria and fungi, Schmidt said.

"There are a lot of areas in the world that haven't been studied from a microbial perspective, and this is one of the main ones," he said. "We're interested in discovering new forms of life, and describing what those organisms are doing, how they make a living."

Schmidt's lab, along with others, is studying how microorganisms travel from one site to another. One common method of microbe transport is through the air -- they're caught up in winds, sucked up into clouds, form rain droplets and then fall back to the ground somewhere else as precipitation.

But on mountains like Volcán Llullaillaco and Volcán Socompa, the high UV radiation and extreme temperatures make the landscape inhospitable to outside microbes. "This environment is so restrictive, most of those things that are raining down are killed immediately," Schmidt said. "There's a huge environmental filter here that's keeping most of these things from growing."

The next steps for the researchers are laboratory experiments using an incubator that can mimic the extreme temperature fluctuations to better understand how any organism can live in such an unfriendly environment. Studying the microbes and finding out how they can live at such an extreme can help set boundaries for life on Earth, Schmidt said, and tells scientists what life can stand. There's a possibility that some of the extremophiles might utilize completely new forms of metabolism, converting energy in a novel way.

Schmidt also is working with astrobiologists to model what past conditions were like on Mars. With their rocky terrain, thin atmosphere and high radiation, the Atacama volcanoes are some of the most similar places on Earth to the Red Planet.

"If we know, on Earth, what the outer limits for life were, and they know what the paleoclimates on Mars were like, we may have a better idea of what could have lived there," he said.

Other paper authors included Andrew King of Ecosystem Sciences, CSIRO Black Mountain in Acton, Australia; Mariá Farías of Laboratorio de Investigaciones Microbiologicas de Lagunas Andinas, Planta Piloto de Procesos Industriales Microbiologicos, CCT, CONICET in Tucuman, Argentina; Preston Sowell of Geomega, an environmental consulting firm in Boulder; and Christian Vitry of Museo de Arqueologia de Alta Montana in Salta, Argentina.

jueves, 19 de enero de 2012

NASA observa que la repetición de La Niña este año ha alcanzado un punto máximo

ORIGINAL: NASA

La última imagen de las alturas de la superficie del mar en el Océano Pacífico del satélite Jason-2 de NASA muestran que la corriente de La Niña está un pico de intensidad. Los amarillos y rojos indican las zonas donde la altura de la superficie del mar es mayor de lo normal (debido al agua caliente), mientras que los azules y morados representan las zonas donde la altura de la superficie del mar es inferior a lo normal (debido al agua fría). El color verde indica condiciones casi normales. Crédito de la imagen: NASA / JPL capa superficial del océano Equipo Topografía
18 de enero 2012

La Niña, "la diva de la sequía," está en su punto máximo, lo que aumenta las probabilidades de que el Noroeste del Pacífico tendrá un clima más tormentoso este invierno y primavera, mientras que el suroeste y el sur de Estados Unidos haya sequías.

Datos de la altura de la superficie del mar de los satélites de la NASA Jason-1 y -2 muestran que la repetición más leve de la la fuerte Niña del año pasado se ha intensificado recientemente, según lo visto en la última imagen del Océano Pacífico por  Jason-2, disponible en: 

La imagen se basa en el promedio de 10 días a partir de los datos centrados en el 8 de enero de 2012. Representa a los lugares donde la altura de la superficie del  el mar Pacífico es superior a la normal (debido al agua caliente) mostrada como amarillo y rojo, mientras que los lugares donde la superficie del mar es inferior a lo normal (debido al agua fría) se muestran en tonos azules y morados. El color verde indica condiciones casi normales. La altura de la superficie del mar en una zona determinada es un indicador de temperatura del océano y otros factores que influyen en el clima.

Este es el segundo año consecutivo que los satélites altimétricos Jason han medido por debajo de lo normal, la altura la superficie del mar en el Pacífico ecuatorial y las alturas del mar inusualmente alta de superficie en el Pacífico occidental.

"Las condiciones están dadas para un invierno tormentoso y húmedo en el noroeste del Pacífico y un invierno seco, sin lluvias, relativamente en el sur de California, el suroeste y el sur de los Estados Unidos", dice el climatólogo Bill Patzert del JPL. "Después de más de una década de los años secos, sobre todo en la cuenca del río Colorado y en el suroeste de Estados Unidos, y sólo dos años de lluvias normales en los últimos seis años en el sur de California, los bajos suministros de agua están al acecho. Este episodio de La Niña podría profundizar la sequía en ya seco sudoeste y también podría empeorar las condiciones que han alimentado los últimos incendios mortales ".

NASA seguirá de cerca esta última La Niña para ver si ha llegado a su pico de invierno se espera o sigue fortaleciéndose.