Some Planetary Perspective

7 06 2008

Update 2: Reader Jesse Michael forwarded me this animated image above, which does a better job than the flawed NASA image or it’s replacement I found below. It takes about a minute to complete the whole sequence, patience.

While looking for something else, I came across this image from the NASA visualization website. I located the hires TIFF image and annotated it as seen below. I also made a desktop wallpaper out of the TIFF file for those interested. It reminded me to remind you all about perspectives, so here is some perspective on size, solar luminosity, and on our planetary energy budget.


Click here for a larger (TIFF format without annotation) image from NASA
Click here for a desktop wallpaper image (1280×1024 JPEG)

UPDATE: It appears that the NASA provided image above , the source of which is from this NASA page, unbelievably, is wrong.  As reader Erik points out, the sun is too large. I initially had some misgivings about the solar size also, but figured NASA wouldn’t possibly botch such a basic comparison. Shades of the Hubble mirror fiasco. 

Here is another image from NASA JPL that appears to be correct:


Click for larger image from JPL
Note: image above is L-R mirrored for comparison to first image.

Note that distance is not to scale, but planetary and solar size is. To get an idea of distance scale, read this excellent example from Kitt Peak Observatory.

A few factoids:

  • It would take about 109 earths to equal the width of the suns diameter (Sun=1.39 million km Earth=12,700 km)
  • Over 1 million Earths would fit inside the Sun’s volume
  • The sun has a total luminosity output of 386 YottaWatts
    (386,000,000,000,000,000,000,000,000 watts, some background here and here)
  • The total luminous energy output received by earth from the sun is 174 PETAWATTS (174,000,000,000,000,000) watts.
  • A 0.1% increase in luminosity dumps an extra 174 trillion watts (174,000,000,000,000) watts into our planetary energy balance.

Graph courtesy of Steve Milloy, www.junkscience.com click for larger image in new window

Data source for graph: http://www1.ncdc.noaa.gov/pub/data/paleo/climate_forcing/solar_variability/lean2000_irradiance.txt

Note: In the graph above, the low flatline from 1645-1715 is the Maunder Minimum, a period of virtually no sunspots, where the historical reports from the northern hemisphere tell a story of dramatic climate change: harsh winters, cools summers, crop failures, famine and disease.

From the abstract referenced above: “Estimated increases since 1675 are 0.7%, 0.2% and 0.07% in broad ultraviolet, visible/near infrared and infrared spectral bands, with a total irradiance increase of 0.2%. “

So its not just 0.1 %, it is 0.2% which translates to a 348 TeraWatts global irradiance increase.

Now lets put 348 trillion watts into perspective:

Hurricanes: the heat energy released by a hurricanes category 1-5 equals about 50 to 200 trillion watts or about the same amount of energy released by exploding a 10-megaton nuclear bomb every 20 minutes.

Katrina, released about 200 trillion watts over its life cycle.

Now imagine double that amount of extra energy being added to earth’s atmosphere every second by small increases in the suns output that have been documented to exist. That’s what the increase in solar irradiance is doing. Since 1675, after the depths of the Maunder Minimum, we’ve seen an increase in solar irradiance of about 2.5 watts per square meter.

Climate modelers say that the extra CO2 equates to a forcing of about 2 watts per square meter, which totals about 1.12 Petawatt (1,120,000,000,000,000 watts). The problem is, they can’t always recreate that reliably between all of the different models out there, with the positive and negative feedback mechanisms, and other variables involved. There’s disagreement on the total contribution. A lot of it. Nonetheless they seem all to agree that CO2 makes some contribution, and that’s likely true. But compared to the sun, I believe it’s minimal.

Now lets look at us: 13.5 TeraWatts is the average total power consumption of the human world in 2001.

Compared to solar variance, do you think we could change the planets atmospheric energy balance with that if we squeezed all the power we made that year together and radiated it into our atmosphere ?

What is very clear though, when you look at history, and the graph above, is that our earths atmosphere and resulting climate is extremely sensitive to variations in solar output. The sweet center point seems to be about 1365 watts per square meter of irradiance…what we consider as “normal” climate. Take 1.5 watts/sq. meter away, and we get significant cooling, harsh winters, cool summers, and increases in ice and glaciers. Add 1.5 watts,/sq. meter and we get hotter summers, mild winters, and melting of ice and glaciers.

Now irradiance aside, as it’s only one component, there’s also the chnage in the suns dynamic magnetic field and solar wind, which according to Svensmark, which modulates the number of cosmic rays that enter our atmosphere (I think there may be some possible effect also due to modulation of the earth’s magnetic field), which modulates the number of clouds that form, hence changing the net surface irradiance. Plots of changes in the suns magnetic field line up very well with climate change.

Here is a little more on perspective and our place in the universe: Read the rest of this entry »





Jason-2 satellite set to launch June 15th from Vandenberg, will track sea level

7 06 2008

Jason-2/Ocean Surface Topography Mission (OSTM).
Jason-2/Ocean Surface Topography Mission (OSTM).
Click for High resolution image (Credit: NOAA)

Hopefully, this will put an end to tide gage data and it’s nuances (such as subsidence). From a  NOAA press release:

A new satellite set to launch next month will monitor the rate of sea-level rise and help measure the strength of hurricanes, according to a leading NOAA scientist.

At a press briefing May 20th, Laury Miller, chief of NOAA’s Laboratory for Satellite Altimetry, said NOAA will use data from the Jason-2/Ocean Surface Topography Mission (OSTM) to extend a 15-year record from two earlier altimeter missions that currently show sea level is rising at a rate of 3.2 mm/year — nearly twice as fast as the previous 100 years. “This rate, if it continues unchanged over the coming decades, will have a large impact on coastal regions, in terms of erosion and flooding,” said Miller.

The Jason-2/OSTM is scheduled for lift off June 15 at 1:47 a.m. from Vandenberg Air Force Base, Calif. The spacecraft is a joint, international effort between NOAA, NASA, France’s Centre National d’Etudes Spatiales (CNES), and the European Organisation for the Exploitation of Meteorological Satellites (Eumetsat).

 Like its predecessor missions TOPEX/Poseidon and Jason-1, Jason-2/OSTM is designed to extend the climate data record by providing a long-term survey of Earth’s oceans, tracking ocean circulation patterns and measuring sea-surface heights and the rate of sea-level rise. These are all key factors in understanding climate change.

The satellite will use a radar altimeter instrument attached to it and fly in a low Earth orbit allowing it to monitor 95 percent of Earth’s ice-free oceans every 10 days.

In addition to detecting climate change factors, Jason-2/OSTM will also be used in the prediction of short-term, severe weather events, such as hurricanes and tropical storms. According to Miller, NOAA will use the altimeter measurements to monitor ocean conditions that trigger changes in the strength of tropical cyclones, as they move over the ocean towards the land. The technique involves mapping the ocean heat content — the fuel that feeds a storm’s intensity — along the storm’s predicted track.

“Using data received in earlier altimeter missions during hurricanes with wind speeds in excess of 155 miles per hour, we’ve been able to reduce our intensity prediction error by an average of five percent – and in some cases as much as 20 percent,” Miller said. “If we increase the accuracy of intensity predictions, we help save lives.”

During the Jason-2/OSTM lifespan, NOAA will work with CNES to handle the complete ground system support. This includes commanding all the satellite’s maneuvers, downloading all the data the satellite captures, and distributing it to weather and climate forecasters, who are monitoring ocean-born storms and phenomena such as El Niño/La Niña and global sea-level rise.

Additionally, Jason-2/OSTM will be the first, newly launched satellite in which NOAA provides ground support from its NOAA Satellite Operations Facility in Suitland, Md. The facility opened in 2007 and houses $50 million worth of high-tech equipment and controls nearly $5 billion in satellites.

“NOAA is definitely up to the challenge of providing smooth, continuous operational support for this mission, which is sure to bring tangible benefits throughout the world,” said Mike Mignogno, program manager for NOAA’s Polar-orbiting Operational Environmental Satellites.

The National Oceanic and Atmospheric Administration, an agency of the U.S. Commerce Department, is dedicated to enhancing economic security and national safety through the prediction and research of weather and climate-related events and information service delivery for transportation, and by providing environmental stewardship of our nation’s coastal and marine resources. Through the emerging Global Earth Observation System of Systems (GEOSS), NOAA is working with its federal partners, more than 70 countries and the European Commission to develop a global monitoring network that is as integrated as the planet it observes, predicts and protects.





Open Thread #2

7 06 2008

Behave yourselves.

Just remember that some comments with links might end up in the spam filter and may take some time before I notice them.





The Hockey Stick returns as web karma

7 06 2008

Looks like a tipping point has been reached. Click graph for details.