Thursday, February 25, 2010

New Meaning to "Eye Tooth"



Did you know that if you go bind it is possible to see with your eye tooth. Yep. No kidding. Look what I have found in medical news.

Nine years ago, Sharron Thornton’s hair and nails fell out, while her skin developed a blistering rash.  Turns out she was suffering from a very rare condition—know as Stevens-Johnson syndrome—caused by a reaction to a medication. She eventually went blind after the cells in her eye died and left corneal scarring.

While her hair and skin grew back, her eyes remained useless. Her condition devastated her: She thought about suicide, and tried a stem cell procedure, but couldn’t be considered for a cornea transplant. Finally she went on a desperate search for any experimental treatment to cure her blindness.

The surgery, Osteo Odonto Kerato Prosthesis (OOKP), involved fitting a living canine tooth with an optical cylinder and transplanting it into the eye cavity.

For the first time in the U.S., surgeons decided to perform this rare procedure to correct corneal scaring. While the procedure has been done a total of 600 times since the 1980s, it’s still pretty complicated: First the surgeons took Thornton’s tooth and part of her jawbone, and made a hole for the prosthetic lens. Then it got weirder: The surgeons implanted the modified tooth into the woman’s chest and left it there for a few months so the two parts could grow together. And finally, the tooth was implanted into her eye.

Not all doctors in the US think this is a good idea. Dr. Ivan Schwab with the American Academy of Ophthalmology told CNN he believes the process is too difficult and the result too disfiguring. There are alternatives that are nearly as good, he added. “We’ve known about the procedure since the ’80s. It’s been going on for a while,” he said. “We’ve viewed it with some skepticism. It requires a sizable team and several operations. It seems to be reasonably successful on the small numbers that have been done,” though it does bring some disfigurement. Enlarge the image to understand how the procedure is done.

A 57 year-old Irish father-of-eight was blinded in a work-place accident, when liquid aluminum exploded in his face in November 2005. "I thought I was going to be blind for the rest of my life. I went to see a professor in Nottingham who was involved in stem cell research and he transplanted some embryonic membrane, but it did not work. He suggested Dr Liu in the Sussex Eye Hospital in Brighton and we took it from there," he said.

They were going to use his eye tooth to transplant but given his age, it was decided that a donor with younger gums would be more suitable. All eight of his children volunteered to provide a tooth, but in the end it was a son who was his namesake that gave his tooth. While the son was having his tooth and part of his gum and lower jaw extracted, his father was being prepared to receive his new eye, which was finally fitted after a total of 16 hours on the operating table. The cost was in the neighborhood of $100,000.

Given the complicated procedure that is involved, Mr. McNichol was told there was just a 65 percent chance of success but, as far as he is concerned, it has been a complete success.

"It doesn't look that great to be honest. People think I look like the Terminator but I don't care. The looks end of it are cosmetic and they don't matter. "What is incredible is that I have come out of darkness into light again. I can watch television. I can walk down the street on my own. I can play darts and pool. I can see my wife and kids. It is just unbelievable"

The surgery which was pioneered in Italy in the 1960’s, is carried out on patients for whom conventional corneal transplants will not work. It entails replacing a damaged cornea with a live tooth root and attached optical cylinder.

As you look at the picture of Mr. McNichol, would you be willing to look like that if you could see again?


Friday, February 19, 2010

A Better Way to FW: (Fwd:)


I receive a goodly number of forwarded e-mails. I bet you do also. Mostly we get them from friends and family. Who else is going to bother? It’s a great way to share things of interest. We enjoy getting these but sometimes they are quite messy with a lot of Fw:s, like this:

 Subject: Fw: Fwd: Fwd:Fwd:Fwd:Fwd:

----- Forwarded Message ----
From: "xxxxxxxxxxt"
To: xxxx xxxxO.COM>; xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>

Sent: Mon, February 15, 2010 4:24:58 PM
Subject: Fwd: XXXXXXXXXXXXXXXXXXXXXXXX
----- Forwarded Message ----
From: "xxxxxxxxxxt"
To: xxxx xxxxO.COM>; xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>

Sent: Mon, February 16, 2010 4:24:58 PM
Subject: Fwd: XXXXXXXXXXXXXXXXXXXXXXXX

----- Forwarded Message ----
From: "xxxxxxxxxxt"
To: xxxx xxxxO.COM>; xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>

Sent: Mon, February 17, 2010 4:24:58 PM
Subject: Fwd: XXXXXXXXXXXXXXXXXXXXXXXX

 ----- Forwarded Message ----
From: "xxxxxxxxxxt"
To: xxxx xxxxO.COM>; xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>xxxx xxxxO.COM>

Sent: Mon, February 18, 2010 4:24:58 PM
Subject: Fwd: XXXXXXXXXXXXXXXXXXXXXXXX

Much of this information is filled in with names and e-mail addresses of people you don’t even know. These people may not know that their names and e-mail addresses are being sent out into cyberspace without their knowledge. Sometimes we have to click through several levels of pages to even get to the message intended to be seen.

If you are at the end of such a sharing chain, you'll quickly see why cleaning up e-mails before forwarding them is essential: messages that have been forwarded multiple times often contain '>' and other quotation characters in all the wrong places, lines are broken in even worse places, and email addresses of people you don't want to know are everywhere.
Cleaning up such a mess can be cumbersome, but keeping an e-mail clean that you forward initially is easy.
  • First, make sure you're sharing the e-mail, not the addresses in it by removing all addresses from the forwarded message. Here is how to do that:
    • Hit your forward button, but don’t send yet.
    • Next, highlight all the extraneous address information and hit “delete.”  Like magic, they are gone.
  • Then, clean up the message itself if it contains unnecessary '>' characters or messed up line breaks. You can do that this way:
    • You can delete all the unnecessary symbols one at a time, or you can use you systems Find and Replace feature by entering the symbol (like “>”) and replace with a blank space by hitting the space bar. This will replace them all at one time.
o       Place any comments you have after or (preferably) before the forwarded message, but try to avoid mixing forwarded text and comments.
  • Now, you are ready to send just the information you want to forward.

Respect privacy and take care not to share others' e-mail addresses without permission. If you send or forward a mass e-mail, with addresses in the To: ___ or Cc: ___ fields, you are compromising their privacy, and possibly alienating them. If you have the slightest doubt about exposing addresses, put them in the blind carbon copy, or Bcc: ___ field. (Most e-mail clients have a link to the Bcc: behind the To: ___field.) This is especially true if you are doing a mass mailing yourself. So that each recipient will not see the addresses of the others, put all but one of the addresses in the Bcc: ___field.

Another breach of email privacy is emailing people you don't know, unless you can name a person that referred you to them.

Do these things and your e-mail friends will be happy you send such clean e-mails. You may wish to pass this information to them as well.

Monday, February 15, 2010

What about Global Warming?

If you are like me, when something crosses your mind that you wonder about, you go research it to the best of your ability. Everyone has an opinion, but what about the data to support it? Let’s look at this business of weather and climate. Is there a difference between the two? There are some terms we need to define to understand what we are talking about.

Think of weather as a brief snapshot of activity and climate as the overall picture. More technically, weather is the state of atmosphere-ocean-land conditions (hot/cold, wet/dry, calm/stormy, sunny/cloudy) that exist over relatively short periods like hours or days. Weather includes the passing of a thunderstorm, a hurricane, blizzard or a cold snap, hot or cold days, severe storm events or clear days. Weather variability and extreme events may respond unpredictably in response to climate change. 

We generally look at Climate as Tropical, Dry, Temperate, Cold and Polar. Climate is the characteristic condition of the atmosphere near the earth's surface at a certain place on earth. It is the long-term weather of that area (at least 30 years). This includes the region's general pattern of weather conditions, seasons and weather extremes like hurricanes, droughts, or rainy periods. Two of the most important factors determining an area's climate are air temperature and precipitation.

Let’s look first at what causes our weather patterns, then at the elements affecting climate. If we look at weather news (I suppose all of  us do) then we have heard the terms like El Niño, La Niña, The Gulf Stream, The Jet Stream, highs and lows, warm front, cold fronts, etc.

Our weather in the United States moves from west to east. This is principally due to the earth’s rotation. It starts somewhere in the Pacific Ocean and crosses the country. It is said that we are currently under the influence of El Niño

El Niño is characterized by unusually warm ocean temperatures in the Equatorial Pacific, as opposed to La Niña, which is characterized by unusually cold ocean temperatures in the Equatorial Pacific. El Niño is an oscillation of the ocean-atmosphere system in the tropical Pacific having important consequences for weather around the globe. One consequence is increased rainfall across the southern tier of the US. We have certainly seen that of late.

The impacts of El Niño and La Niña at these latitudes are most clearly seen in wintertime. In the continental US, during El Niño years, temperatures in the winter are warmer than normal in the North Central States, and cooler than normal in the Southeast and the Southwest. During a La Niña year, winter temperatures are warmer than normal in the Southeast and cooler than normal in the Northwest

El Niño is Spanish for “the little boy” or “Christ child.” This warm deep-water ocean current was discovered by fisherman long ago off the north-west coast of South America. It is called the “Christ child” because it begins around December 25th.  La Niña means “the little girl” in Spanish. But it is also referred to as El Viejo, “the old one.”

If weather patterns change and persist over time, the climate is subject to change. Let’s look at the things that influence our climate.

Latitude
The latitude of an area—that is, its distance from the Equator—determines the amount of heat it receives from the sun. Close to the Equator, the sun's rays fall nearly vertically on the earth's surface most of the year. North or south of the tropics, the rays always reach the earth at a slant. Where the rays fall at a slant, they provide less warmth because they are spread out over a larger area.

Altitude
As the altitude, or height above sea level, increases, the temperature decreases at a rate of about 1 degree F. for each 300 feet. The thinner air at higher altitudes does not hold the heat radiated from the earth; this heat escapes into space. Even near the Equator, the climate at high altitudes may be extremely cold, as on Africa's snowcapped Mount Kenya.

Winds
Prevailing winds carry the heat and moisture content of the areas where they originate to other areas. The winters of Sitka, in southern Alaska, because of southwesterly winds off the warm Pacific Ocean, are as warm as those of Philadelphia, 1,000 miles closer to the Equator.
 
Large Bodies of Water
A body of water heats and cools much less rapidly than land does. A large body of water, therefore, provides a cooling effect in the summer and a warming effect in the winter, particularly where the prevailing winds blow onshore. In contrast, areas of land far from any large body of water tend to have larger temperature variations with the seasons. For example, the difference between the average temperatures of the warmest and coldest months in San Francisco, on the Pacific Ocean, is only 11 degrees F. In Kansas City, Missouri the difference is 51 degrees F.

Now that we know a little about our weather and climate, what about the question at hand concerning global warming.  Temperatures on land and sea began to be taken around the world about 1854, but not until 1880 were there enough measuring posts to be effective for gauging climate. We then developed some 8,000 locations where daily temperatures are taken. We have kept track of temperatures for the last 130 years. So what have we learned?

According to the National Oceanic and Atmospheric Association (NOAA), our global temperature has been on the rise for the last thirty years (Note the chart from the National Climatic Data Center) which shows the annual global temperature anomalies. The term “temperature anomaly” means a departure from a reference value or long-term average. A positive anomaly indicates that the observed temperature was warmer than the reference value, while a negative anomaly indicates that the observed temperature was cooler than the reference value.

According to the scientific data, the earth seems to be getting warmer. OK, so what? Does this have any effect on us? Besides the fact they we may sweat a little more, it can have far reaching effects. How is that? It seems pretty cold right now in parts of the country that should be warmer. How does that reconcile with a warming climate?

Go back to our photo analogy. Zoom in on the top of a photograph and you see a snow covered mountain. Zoom in on the bottom and you see a warm sandy beach. Zoom out and you see the whole picture containing both views. The outward zoom is the climate. The inward zoom is the weather. Gradual changes in the climate can cause extreme changes in the weather, both hot and cold. Never before in the history of records has all 50 states had snow on the ground  at the same time, as happened on February 12th of this year.

Ocean currents also play an important part in determining climate. They carry heat from the tropics toward the poles. For example, the warm waters of the Gulf Stream help keep the British Isles and northwestern Europe much warmer during the winter than they would otherwise be, giving them mild seasons. The same is true of the east coast of the US. (See map of Gulf Stream.) Is this warm Gulf Stream subject to change? If so, what can happen?


It has been reliably shown that the polar ice caps are melting at an alarming rate. Arctic sea ice extent, which is measured from passive microwave instruments onboard NOAA satellites, usually expands during the cold season to a March maximum, then contracts during the warm season to a September minimum. According to NOAA's National Snow and Ice Data Center, the September Northern Hemisphere average sea ice extent was 23.8 percent below the 1979-2000 average—the third lowest since satellite records began in 1979, behind 2007 and 2008.

The past five years have had the five smallest minimum sea ice extent on record. The September 2009 Arctic sea ice extent was 1.1 million square kilometers greater than 2007's record low and 690,000 square kilometers greater than September 2008, the second-lowest extent. This was the 13th consecutive September with sea ice extent below average. September 1996 was the last year with above-average sea ice extent.

Quoting an article by Thom Hartman (See reference below) here's how it works.

In quick summary, if enough cold, fresh water coming from the melting polar ice caps and the melting glaciers of Greenland flows into the northern Atlantic, it will shut down the Gulf Stream, which keeps Europe and northeastern North America warm. The worst case scenario would be a full blown return of the last ice age in a period as short as 2 to 3 years from its onset and the mid-case scenario would be a period like the "little ice age" of a few centuries ago that disrupted worldwide weather patterns leading to extremely harsh winters, droughts, worldwide desertification, crop failures, and wars around the world.

If you look at a globe, you'll see that the latitude of much of Europe and Scandinavia is the same as that of Alaska and permafrost locked parts of northern Canada and central Siberia. Yet Europe has a climate more similar to that of the United States than northern Canada or Siberia. Why?

It turns out that our warmth is the result of ocean currents that bring warm surface water up from the equator into northern regions that would otherwise be so cold that even in summer they'd be covered with ice. The current of greatest concern is often referred to as "The Great Conveyor Belt," which includes what we call the Gulf Stream.

The Great Conveyor Belt, while shaped by the Coriolis effect of the Earth's rotation, is mostly driven by the greater force created by differences in water temperatures and salinity. The North Atlantic Ocean is saltier and colder than the Pacific, the result of it being so much smaller and locked into place by the Northern and Southern American Hemispheres on the west and Europe and Africa on the east. As a result, the warm water of the Great Conveyor Belt evaporates out of the North Atlantic leaving behind saltier waters, and the cold continental winds off the northern parts of North America cool the waters. Salty, cool waters settle to the bottom of the sea, most at a point a few hundred kilometers south of the southern tip of Greenland, producing a whirlpool of falling water that's 5 to 10 miles across. While the whirlpool rarely breaks the surface, during certain times of year it does produce an indentation and current in the ocean that can tilt ships and be seen from space (and may be what we see on the maps of ancient mariners).

This falling column of cold, salt laden water pours itself to the bottom of the Atlantic, where it forms an undersea river forty times larger than all the rivers on land combined, flowing south down to and around the southern tip of Africa, where it finally reaches the Pacific. Amazingly, the water is so deep and so dense (because of its cold and salinity) that it often doesn't surface in the Pacific for as much as a thousand years after it first sank in the North Atlantic off the coast of Greenland.

The out-flowing undersea river of cold, salty water makes the level of the Atlantic slightly lower than that of the Pacific, drawing in a strong surface current of warm, fresher water from the Pacific to replace the outflow of the undersea river. This warmer, fresher water slides up through the South Atlantic, loops around North America where it's known as the Gulf Stream, and ends up off the coast of Europe. By the time it arrives near Greenland, it's cooled off and evaporated enough water to become cold and salty and sink to the ocean floor, providing a continuous feed for that deep sea river flowing to the Pacific. These two flows warm, fresher water in from the Pacific, which then grows salty and cools and sinks to form an exiting deep sea river are known as the Great Conveyor Belt.

So, what do we get from all this? We learn that the weather is stranger than it has been in a very long time. The polar ice is melting. Such events could affect many areas of our planet and thus our life. But the question remains. What is really causing all this change and what are we going to do about it? Is it caused by greenhouse gases or the diminishing forests of the world, or as has been suggested by some, methane gas emission caused by large quantities of cow poop?
I don’t have the answer, but I do lament all the political haranguing attached to the question. The world seems to agree there is a problem. Now, let’s see what we can do to correct it.

References

Christy, John R., R.W. Spencer, and W.D. Braswell, 2000: MSU tropospheric Temperatures: Dataset Construction and Radiosonde Comparisons. J. of Atmos. and Oceanic Technology, 17, 1153-1170.
Free, M., D.J. Seidel, J.K. Angell, J. Lanzante, I. Durre and T.C. Peterson (2005) Radiosonde Atmospheric Temperature Products for Assessing Climate (RATPAC): A new dataset of large-area anomaly time series, J. Geophys. Res., 10.1029/2005JD006169.
Free, M., J.K. Angell, I. Durre, J. Lanzante, T.C. Peterson and D.J. Seidel(2004), Using first differences to reduce inhomogeneity in radiosonde temperature datasets, J. Climate, 21, 4171-4179.
Fu, Q., C.M. Johanson, S.G. Warren, and D.J. Seidel, 2004: Contribution of stratospheric cooling to satellite-inferred tropospheric temperature trends. Nature, 429, 55-58.
Lanzante, J.R., S.A. Klein, and D.J. Seidel (2003a), Temporal homogenization of monthly radiosonde temperature data. Part I: Methodology, J. Climate, 16, 224-240.
Lanzante, J.R., S.A. Klein, and D.J. Seidel (2003b), Temporal homogenization of monthly radiosonde temperature data. Part II: trends, sensitivities, and MSU comparison, J. Climate, 16, 241 262.
Mears, CA, FJ Wentz, 2009, Construction of the RSS V3.2 lower tropospheric dataset from the MSU and AMSU microwave sounders. Journal of Atmospheric and Oceanic Technology, 26, 1493-1509.
Mears, CA, FJ Wentz, 2009, Construction of the Remote Sensing Systems V3.2 atmopsheric temperature records from the MSU and AMSU microwave sounders. Journal of Atmospheric and Oceanic Technology, 26, 1040-1056.
Mars, Carl A., M.C. Schabel, F.J. Wentz, 2003: A Reanalysis of the MSU Channel 2 tropospheric Temperature Record. J. Clim, 16, 3650-3664.
Peterson, T.C. and R.S. Vose, 1997: An Overview of the Global Historical Climatology Network Database.Bull. Amer. Meteorol. Soc., 78, 2837-2849.
Quayle, R.G., T.C. Peterson, A.N. Basist, and C. S. Godfrey, 1999: An operational near-real-time global temperature index. Geophys. Res. Lett., 26, 333-335.
Smith, T. M., and R. W. Reynolds (2004), Improved extended reconstruction of SST (1854-1997), J. Climate, 17, 2466-2477.
Smith, T. M., et al. (2008), Improvements to NOAA's Historical Merged Land-Ocean Surface Temperature Analysis (1880-2006), J. Climate, 21, 2283-2293.
Hartmann, Thom (2004),   How Global Warming May Cause the Next Ice Age, Common Dreams.org.
.The complete land-sea surface climatology from the Climate Research Unit is described in:
Jones, P. D., M. New, D. E. Parker, S. Martin, and I. G. Rigor (1999), Surface Air Temperature and its Changes Over the Past 150 Years, Rev. Geophys., 37(2), 173—199.
Global land areas, excluding Antarctica, described in:
New, M. G., M. Hulme and P. D. Jones, in press: Representing 20th century space-time climate variability. I: Development of a 1961-1990 mean monthly terrestrial climatology. J. Climate.
Global oceans, 60S-60N, described in:
Parker, D. E., M. Jackson and E. B. Horton, 1995: The GISST2.2 sea surface temperature and sea-ice climatology. Climate Research Technical Note, CRTN 63, Hadley Centre for Climate Prediction and Research, Bracknel, UK.
Arctic sea areas, described in:
Rigor, I. G., R. L. Colony and S. Martin, submitted: Statistics of surface air temperature observations in the Arctic. J. Climate.
Martin, S. and E.A. Munoz: Properties of the Arctic 2-Meter Air temperature field for 1979 to the present derived from a new gridded data set. J. Climate, 10, 1428-1440.

Wednesday, February 10, 2010

Why Just 28 days in February?

February didn’t use to be in the calendar at all, neither did January. The early calendars were only ten months long (304 days), beginning with March as the first month. As far as the ancients were concerned, winter was lost time. Nothing happened in the cold months. The calendar was an agricultural and lunar cycle concern. Apart from knowing when to plant, why did one need to count the days?

January and February were added to make the twelve months. Every other year, February was shortened and a leap month (Intercalaris) was added in an attempt to realign lunar cycles with the solar calendar. The lengths of the years in a four year cycle of this lunisolar calendar were 355, 377, 355, and 378 days. This added up to 4 days too many to stay in sync with the solar year.


Eventually Julius Caesar asked an astronomer, Sosigenes of Alexandria, Egypt, to devise a better calendar. He abandoned aligning the months with lunar cycles, and adopted months of 30 or 31 days length, keeping February at 28 days. He introduced an extra day in February in leap years. The calendar year was realigned to begin with January.  What resulted is called the Julian Calendar.


Julius Caesar re-named the 5th month (when March was the first month) after himself. His successor, Augustus Caesar, re-named the 6th month after himself.


The first day of each month was called Kalendae, or calends. Debts were due on this day, so books to track payments were called calendarium (account book) from which we get our modern day calendar. The name of the month comes from the Latin Februarius “of Februa.” Februa was a Roman festival of purification held on February fifteenth.


Remember, February was the last month of the year when it was created. It needed only enough even days to fill out the 365 day calendar.


The origin of the names for the other months of the year is as follows:

January: Latin Januarius mensis "month of Janus"
Janus is the Roman god of gates and doorways, depicted with two faces looking in opposite directions. His festival month is January. Januarius had 29 days, until Julius Caesar when it became 31 days long.

March: Latin Martius "of Mars." March was the original beginning of the year, and the time for the resumption of war. Mars is the Roman god of war.


April: Latin Aprilis  Greek Aphro, short for Aphrodite, goddess of love and beauty. She is identified with the Roman goddess Venus.

May: Latin Maius "of Maia."  Maia (meaning "the great one") is the Italic goddess of spring, the daughter of Faunus, and wife of Vulcan.


June:  Latin Junius "of Juno."  Juno is the principle goddess of the Roman Pantheon. She is the goddess of marriage and the well-being of women. She is the wife and sister of Jupiter.


July: Latin Julius "Julius." Julius Caesar reformed the Roman calendar (hence the Julian calendar) in 46 BC. In the process, he renamed this month after himself.

August:  Latin Augustus "Augustus."  Augustus Caesar clarified and completed the calendar reform of Julius Caesar. In the process, he also renamed this month after himself.


September, October, November and December are the numbered months for the Latin: septem, “seven”; octo, “eight”; novem, “nine” and decem, “ten.” We know that September is the ninth month in our calendar etc., but remember the months were named during the time when the first month was March.