nearingzero/nz393.jpe - PowerPoint PPT Presentation

slide1 n.
Skip this Video
Loading SlideShow in 5 Seconds..
nearingzero/nz393.jpe PowerPoint Presentation
Download Presentation

play fullscreen
1 / 71
Download Presentation
Download Presentation


- - - - - - - - - - - - - - - - - - - - - - - - - - - E N D - - - - - - - - - - - - - - - - - - - - - - - - - - -
Presentation Transcript


  2. el Niño Any comments on the video? Sorry about the crummy quality. I looked for a place to buy a good copy of the video; no luck. Why are video makers so enamored of gloom and doom? “Next to the changing of the seasons, el Niño has the greatest influence on the Earth’s climate.” This is something big, and we ought to understand it. “Climate is what we expect. Weather is what we get.“—Robert Heinlein

  3. el Niño—Lecture Outline What is it? What causes it? How does it affect us? Can we change it? What’s happening today? El Niño in the future?

  4. el Niño—what is it? I obtained the information in this lecture from a number of web sites. The links are listed at the end of this lecture. I’ll do my best to give proper credit when I use somebody else’s words or pictures. I’ll be glad to correct any omissions. “El Niño is an intermittent disruption of the climate system centered in the equatorial Pacific.”1 We now know it has effects on weather across much of the world. maybe skip to slide 9.

  5. Digression: Global Circulation Patterns “Air rises near the equator, where it is hottest, and sinks near the poles, where it is cooler. However, instead of a circulating in a single loop in each hemisphere, the motion divides into three cells in the northern and three in the southern hemisphere.” convection (coming soon in a demo) “The wind does not blow straight north or south between the bands of rising or falling air; the Coriolis effect bends winds to the right in the Northern Hemisphere and to the left in the Southern.” surface winds (coriolis effect) “Trade Winds” from (link now dead); also see this site

  6. Digression: Coriolis “Force” The Coriolis effect is the term used to describe the apparent motion of an object relative to a rotating reference frame. Let’s aim a big cannon at the North Pole towards a target on the equator. Remember: an object in motion moves in a straight line unless acted on by an external force. Will we hit the target? (link now dead) For you nitpickers in the audience, yes, the cannonball will follow a parabolic trajectory under the influence of gravity. We would need to calculate the correct firing angle that would allow the cannonball to hit at the equator.

  7. We miss every time. There must be a force deflecting the cannonball. The “Coriolis Force.” Right? Wrong. The earth rotates “out from underneath” the cannonball. The target moves. The cannonball goes in a straight line. An observer in the rotating (accelerated) reference frame of the earth “invents” a fictitious “Coriolis” force to explain the apparent deflection (like “centrifugal force”).

  8. Imagine throwing a ball to a friend on a rotating merry-go-round. throw a ball it goes “straight” appears to curve Here’s a little movie. Here is the external link (for viewing on a computer other than mine). (Looks to my eyes like friction is causing the ball to move in a curved path as it slows down.) Does the Coriolis effect cause your bathwater to rotate clockwise as it drains? No. Bad coriolis. More technical “stuff” on the Coriolis effect (broken link, 2012).

  9. back to el Niño “El Niño is an unusual warming of the tropical Pacific Ocean that occurs irregularly at about 3-6 year intervals in response to large scale weakenings of the trade winds that normally blow westward from South America toward Asia.”2 “normal” el Niño onset

  10. 3

  11. “El Niño…

  12. La Niña, suggested on the slide before last, is the “opposite” of el Niño. • el Niño—the warm western Pacific waters move eastward towards the Americas • la Niña—the waters off the Americas are cooler than normal • there is debate2 over whether la Niña represents “normal” conditions, with “in between” being the buildup towards el Niño… • or whether the “in between” buildup towards el Niño is “normal”

  13. The 1997-1998 event.3 “normal” el Niño developing la Niña

  14. Reminds me of water sloshing in a bathtub.

  15. Click here (on my computer) or on the link below to see the thermocline animation. (dead link) (2012)

  16. A couple of nitpicky clarifications, to satisfy my conscience… 1. I’m OK if you want to think of the trade winds as pushing water from East to West. Mental models help our under-standing. The reality is more complex. 2. Ocean waves don’t carry water molecules from one end of the ocean to the other. One consequence is that waves can travel much faster than “pieces” of water.

  17. Historical records of el Niño date back to at least 1567. a sampling of el Niño events “The name El Niño (referring to the Christ child) was originally given by Peruvian fisherman to a warm current that appeared each year around Christmas. What we now call El Niño seemed to them like a stronger event of the same type, and the usage of the term changed to refer only to the irregular strong events. It wasn't until the 1960s that it was widely realized that this was not just a local Peruvian occurrence, but was associated with changes over the entire tropical Pacific and beyond.”1

  18. In 1904, Sir Gilbert Walker, head of the Indian Meter-ological Service, began attempts to predict India’s monsoons, on which the survival of millions depends. “He recognized some patterns of rainfall in South America and associated them with changes in ocean temperatures. He also found a connection between barometer readings at stations on the eastern and western sides of the Pacific.”4 According to Walker (1923) "when pressure is high in the Pacific Ocean it tends to be low in the Indian Ocean from Africa to Australia." “Changes across the tropical Pacific and beyond are not isolated phenomena but are connected as part of a larger oscillation.”1

  19. “When pressure is high in the Pacific Ocean it tends to be low in the Indian Ocean from Africa to Australia." Darwin: Australia Tahiti: closer to South America Walker was ridiculed for suggesting that there is a connection between monsoons in India and mild winters in Canada.4

  20. In the 1960’s, Jacob Bjerknes, at the University of California, was the first to see a connection between unusually warm sea-surface temperatures and the weak easterlies and heavy rainfall that accompany low pressure in Darwin. Ultimately, Bjerknes' discovery led to the recognition that the warm waters of El Niño and the pressure seesaw of Walker's Southern Oscillation are part of the same phenomenon -- sometimes referred to by the acronym ENSO.4 ENSO—“El Niño/Southern Oscillation” “Oscillation” makes me think of something vibrating back and forth with periodic motion.

  21. el Niño—what causes it? This web page says “el Niño is where the normal circulation patterns of the atmosphere and ocean in the Southern Pacific break down and may even reverse.  La Niña on the other hand, is an abnormal strengthening of that normal circulation.” They are the experts, not me, but it seems that the entire el Niño/la Niña cycle is a normal part of the Earth’s “life.” Earlier I wrote that el Niño was a response to weakening of the trade winds. But why should the trade winds weaken?

  22. “There are more things in heaven and Earth, Horatio, than are dreamt of in your philosophy.”—Hamlet It is clear that over time warm water piles up in the Western Pacific. This is an unstable situation, waiting for a “trigger” to release the pent-up water. The weakening of the trade winds is certainly one trigger... …but there are other natural phenomena that affect ocean water. You are familiar with the jet stream, which is related to the global circulation patterns I showed earlier.

  23. The jet stream is an example of an atmospheric Rossby wave.

  24. There are oceanic Rossby waves in the Pacific. Click on the picture to see a movie. For those not using my computer, click here to view the movie from its source web site (link dead 2012). Rossby waves, like the trade winds, are caused by the Coriolis effect.

  25. The “waves” are typically 5 centimeters in height and take months to years(dead link) to cross the Pacific from east to west. (Alternative link: ) Rossby waves reflecting from the continents of the Western Pacific may have something to do with triggering el Niño… …but not in all cases (see heredead link). (updated links: ; )

  26. Volcanoes do not cause el Niños… …but there is a correlation between major tropical volcanic eruptions and occurrences of el Niño. “There was a nearly one-in-two chance of an El Niño event occurring after a volcanic eruption in the tropical zone, roughly double the normal probability.” “It appears that the eruption of a tropical volcano nudges the climate towards a more El Niño-like state.”—Michael Mann, University of Virginia.

  27. “Since El Niños occur against the background existing climate, there is little doubt that volcanic eruptions that eject large amounts of dust into the stratosphere must modify the frequency, character and strength of El Niño events, possibly in important ways.” “The distinction I make is between "slowly modify the background" and "cause" El Niño.”1

  28. There are also oceanic Kelvin waves that, in contrast to Rossby waves, move from West to East. The red band in this picture indicates above-average sea level water that took a month to travel 1/3 of the way around the world, from Australia to South America. (link dead 2012) Kelvin waves are not el Niños (a month to travel across the Pacific, compared to many months for the lifetime of an el Niño), but may contribute as a “trigger.”

  29. Some of us like to think that if we knew the position and momentum of every molecule in the atmosphere, and all the energy sources and sinks, and everything else that enters into laws of physics… …and had a powerful enough computer… …then we could predict future weather with certainty. It is possible that weather is chaotic—that even absolute knowledge of current conditions would not allow us to predict future weather. (dead link 2012) prediction 1 prediction 1 initial conditions infinitesimally modified Comforting, or frightening?

  30. “El Niños involve the full complexity of ocean-atmosphere interaction on a global scale.” “When you consider longer-term phenomena like El Niño… one must consider how the ocean will evolve under the winds, and then how the altered ocean will modify the winds, and so on, in many tricky and sensitive feedback loops.” In other words, we don’t really know what “causes” el Niño! If it makes you feel any better, we do know that sea beavers don’t cause el Niños.

  31. I’ve made some statements that should wake you up: • “…a tropical volcano nudges the climate towards a more El Niño-like state…” • “…many tricky and sensitive feedback loops…” • “…initial conditions infinitesimally modified (can cause dramatic differences in outcomes).” Do you see why?

  32. el Niño—how does it affect us?                floods, mudslides cyclones coral reefs die drought, crop failure no fish fires downpours, tornados great fishing

  33. la Niña—how does it affect us?

  34. “La Niña often features drier than normal conditions in the Southwest in late summer through the subsequent winter. Drier than normal conditions also typically occur in the Central Plains in the fall and in the Southeast in the winter. In contrast, the Pacific Northwest is more likely to be wetter than normal in the late fall and early winter with the presence of a well-established La Niña. Additionally, on average La Niña winters are warmer than normal in the Southeast and colder than normal in the Northwest.”

  35. Not all the effects of el Niño are bad. 1997, US: • California suffered more than $1.1 billion in economic losses • midwest and East Coast natural gas and heating oil demand reduced by 10 percent—a savings of about $6.7 billion • retail sales in the US about $5.6 billion higher than normal because of the milder winter • more home construction • fewer transportation delays and less salt used on roads

  36. el Niño—can we change it? Is that the “right” question to ask? Should we instead ask “would we want to change it?” Let’s suppose we want to cause an el Niño. NOAA scientist Billy Kessler has some calculations for us to consider. He calculated the energy it would require to heat this water by the 1.62˚C average for el Niño 1997.

  37. You take the surface area of the water (remember, the area covers the length of the Pacific Ocean) times the depth of the affected region to calculate the volume of water heated. V = A D The mass of water is volume times density: m =  (A D) The energy required is the mass times the heat capacity times the temperature change (you had a similar homework assignment) E = [ (A D)] C T

  38. Kessler estimates that 3.5x1022 joules of energy would be needed. That’s 3,500,000,000,000,000,000,000 joules. That’s a ton of joules, isn’t it! Wrong! It is the equivalent of 389 tonnes of mass.

  39. 3,500,000,000,000,000,000,000 joules. Kessler calculates that amount of energy would be released by 400,000 twenty-megaton hydrogen bombs. The bomb that destroyed Hiroshima was a 10 kiloton atomic bomb. The energy “tied up” in an el Niño is “worth” about 800,000,000 Hiroshima bombs.

  40. Kessler correctly points out that el Niño actually involves a movement of already-heated water, rather than the heating of the water itself… …which, give or take a few factors of 10, would require “the same” energy as the result I just showed… …which he also shows is equivalent to 1,500,000 huge (1000 MW) power plants operating round-the-clock for 8 months. Alternatively, you could disrupt el Niño by dissolving a 1 km square, 100 km high “chunk” of salt in the surface water, which would cause the warm surface water to cool and sink. There is a “wild card,” which I will discuss later. The ability to forecast el Niño in advance would allow us to take steps to save lives and money.

  41. Actually, we can see that el Niño is coming about 6 months before major changes take place. That warning could be used for emergency preparations... …except we can’t predict in advance the specific weather events that will cause disasters. And we can’t move thousands of people away from their homes in anticipation of a disaster that is unlikely to happen.

  42. el Niño—what’s happening today? The TAO buoy array (we saw some of the buoys in the video) covers a vast stretch of the Pacific Ocean centered on the equator, from north of Australia almost to South America. TAO: “Tropical Atmosphere-Ocean” updated for 2012

  43. These buoys provide continual sea surface temperature (SST) and wind data. The figure above shows the most recent 5-day average SST and winds, as of March 14, 2012. Updates are here.