miércoles, 4 de mayo de 2011

NASA: Artic Sea Ice - 03-05-11


Open your mind, your heart to other cultures
Abra su mente, su corazón a otras culturas
You will be a better person
Usted será una mejor persona
RM

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Layers of frozen sea water, known as sea ice, cap the Arctic Ocean. The ice grows dramatically each winter, and melts just as dramatically each summer. In the past decade, the melting has grown more dramatic, while growth has become less so, as you can see in our World of Change feature.
The pair of images above shows Arctic sea ice concentrations for September 2010 (left) and March 2011. The yellow outline shows the median sea ice extent observed by satellite sensors in September and March from 1979–2000. “Extent” is the total area with an ice concentration of at least 15 percent. The maps were compiled from observations by the Defense Meteorological Satellite Program and by the Advanced Microwave Scanning Radiometer for EOS (AMSR-E), on NASA’s Aqua satellite. The sensors measure microwave energy radiated from Earth’s surface, as sea ice and open water emit microwaves differently.
On September 19, 2010, Arctic sea ice reached its annual minimum, at 4.60 million square kilometers (1.78 million square miles). The National Snow and Ice Data Center (NSIDC) declared 2010 to be the third-lowest Arctic sea ice extent in the satellite record.
In March 2011, after a winter of growth, sea ice extent in the Arctic was the second lowest for the month of March since satellite records were first kept in 1979. NSIDC reported the overall ice extent at 14.56 million square kilometers (5.62 million square miles) at the maximum on March 7. Concentrations remained below normal in both the Atlantic and Pacific sectors of the Arctic, particularly in the Labrador Sea and the Gulf of St. Lawrence.
New data showed that the amount of older, thicker ice had increased slightly over last year. “Data through the third week of March shows an increase in sea ice one to two years old, and older than two years old, compared to recent years,” NSIDC noted. “However, the amount of older ice remains much lower than in the mid-1980s, and there is still almost none of the oldest ice (older than four years) that used to dominate much of the Arctic Ocean.”
Including 2011, the March trend in sea ice extent has been decreasing at a rate of 2.7 percent per decade. Visit World of Change: Arctic Sea Ice to see the trend since 1999.
NASA Earth Observatory image by Jesse Allen, using data from the National Snow and Ice Data Center (NSIDC). Caption by Mike Carlowicz.

Instrument: 
DMSP - SSM/I



NASA: Artic Sea Ice - 03-05-11



You have an alphabetical guide in the foot of the page in the blog: solitary dog sculptor
In the blog: Solitary Dog Sculptor I, the alphabetical guide is on the right side of the page
Thanks

Usted tiene una guía alfabética al pie de la página en el blog: solitary dog sculptor
En el blog: Solitary Dog Sculptor I, la guia alfabética está en el costado derecho de la página
Gracias




Ricardo M Marcenaro - Facebook

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Solitary Dog Sculptor I:
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My blogs are an open house to all cultures, religions and countries. Be a follower if you like it, with this action you are building a new culture of tolerance, open mind and heart for peace, love and human respect.

Thanks :)

Mis blogs son una casa abierta a todas las culturas, religiones y países. Se un seguidor si quieres, con esta acción usted está construyendo una nueva cultura de la tolerancia, la mente y el corazón abiertos para la paz, el amor y el respeto humano.

Gracias :)




2 comentarios:

  1. impresionante, lo compartí con mis colegas de oficina. Sin embargo es triste revisar los archivos de noticias de la década del 60 y ver que ya se hablaba de esto, de la amazonía, de los bosques, de la energía solar, de tanto a lo cual poco caso le hemos hecho.
    En fin...
    abrazo,
    hj

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  2. El tema es que la situación empeora y nadie quiere ordenar, bajar el ritmo de ompetencias. Nadie quiere dejar de consumir tampoco, también viene desde la gente, no solo los gobiernos.
    Abrazos :)
    RM

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