Archive for April, 2009

Now What? Now Prepare For Dangerous Global Cooling?

Tuesday, April 28th, 2009
Read the sunspots
The mud at the bottom of B.C. fjords reveals that solar output drives climate change - and that we should prepare now for dangerous global cooling
R. TIMOTHY PATTERSON, Financial Post
Published: Wednesday, June 20, 2007
Politicians and environmentalists these days convey the impression that climate-change research is an exceptionally dull field with little left to discover. We are assured by everyone from David Suzuki to Al Gore to Prime Minister Stephen Harper that the science is settled. At the recent G8 summit, German Chancellor Angela Merkel even attempted to convince world leaders to play God by restricting carbon-dioxide emissions to a level that would magically limit the rise in world temperatures to 2C.

The fact that science is many years away from properly understanding global climate doesn’t seem to bother our leaders at all. Inviting testimony only from those who don’t question political orthodoxy on the issue, parliamentarians are charging ahead with the impossible and expensive goal of stopping global climate change. Liberal MP Ralph Goodale’s June 11 House of Commons assertion that Parliament should have a real good discussion about the potential for carbon capture and sequestration in dealing with carbon dioxide, which has tremendous potential for improving the climate, not only here in Canada but around the world, would be humorous were he, and even the current government, not deadly serious about devoting vast resources to this hopeless crusade.

Climate stability has never been a feature of planet Earth. The only constant about climate is change; it changes continually and, at times, quite rapidly. Many times in the past, temperatures were far higher than today, and occasionally, temperatures were colder. As recently as 6,000 years ago, it was about 3C warmer than now. Ten thousand years ago, while the world was coming out of the thou-sand-year-long Younger Dryas cold episode, temperatures rose as much as 6C in a decade — 100 times faster than the past century’s 0.6C warming that has so upset environmentalists.

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(See hardcopy for Chart/Graph)
Andrew Barr, National Post
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Climate-change research is now literally exploding with new findings. Since the 1997 Kyoto Protocol, the field has had more research than in all previous years combined and the discoveries are completely shattering the myths. For example, I and the first-class scientists I work with are consistently finding excellent correlations between the regular fluctuations in the brightness of the sun and earthly climate. This is not surprising. The sun and the stars are the ultimate source of all energy on the planet.

My interest in the current climate-change debate was triggered in 1998, when I was funded by a Natural Sciences and Engineering Research Council strategic project grant to determine if there were regular cycles in West Coast fish productivity. As a result of wide swings in the populations of anchovies, herring and other commercially important West Coast fish stock, fisheries managers were having a very difficult time establishing appropriate fishing quotas. One season there would be abundant stock and broad harvesting would be acceptable; the very next year the fisheries would collapse. No one really knew why or how to predict the future health of this crucially important resource.

Although climate was suspected to play a significant role in marine productivity, only since the beginning of the 20th century have accurate fishing and temperature records been kept in this region of the northeast Pacific. We needed indicators of fish productivity over thousands of years to see whether there were recurring cycles in populations and what phenomena may be driving the changes.

My research team began to collect and analyze core samples from the bottom of deep Western Canadian fjords. The regions in which we chose to conduct our research, Effingham Inlet on the West Coast of Vancouver Island, and in 2001, sounds in the Belize-Seymour Inlet complex on the mainland coast of British Columbia, were perfect for this sort of work. The topography of these fjords is such that they contain deep basins that are subject to little water transfer from the open ocean and so water near the bottom is relatively stagnant and very low in oxygen content. As a consequence, the floors of these basins are mostly lifeless and sediment layers build up year after year, undisturbed over millennia.

Using various coring technologies, we have been able to collect more than 5,000 years’ worth of mud in these basins, with the oldest layers coming from a depth of about 11 metres below the fjord floor. Clearly visible in our mud cores are annual changes that record the different seasons: corresponding to the cool, rainy winter seasons, we see dark layers composed mostly of dirt washed into the fjord from the land; in the warm summer months we see abundant fossilized fish scales and diatoms (the most common form of phytoplankton, or single-celled ocean plants) that have fallen to the fjord floor from nutrient-rich surface waters. In years when warm summers dominated climate in the region, we clearly see far thicker layers of diatoms and fish scales than we do in cooler years. Ours is one of the highest-quality climate records available anywhere today and in it we see obvious confirmation that natural climate change can be dramatic. For example, in the middle of a 62-year slice of the record at about 4,400 years ago, there was a shift in climate in only a couple of seasons from warm, dry and sunny conditions to one that was mostly cold and rainy for several decades.

Using computers to conduct what is referred to as a time series analysis on the colouration and thickness of the annual layers, we have discovered repeated cycles in marine productivity in this, a region larger than Europe. Specifically, we find a very strong and consistent 11-year cycle throughout the whole record in the sediments and diatom remains. This correlates closely to the well-known 11-year Schwabe sunspot cycle, during which the output of the sun varies by about 0.1%. Sunspots, violent storms on the surface of the sun, have the effect of increasing solar output, so, by counting the spots visible on the surface of our star, we have an indirect measure of its varying brightness. Such records have been kept for many centuries and match very well with the changes in marine productivity we are observing.

In the sediment, diatom and fish-scale records, we also see longer period cycles, all correlating closely with other well-known regular solar variations. In particular, we see marine productivity cycles that match well with the sun’s 75-90-year Gleissberg Cycle, the 200-500-year Suess Cycle and the 1,100-1,500-year Bond Cycle. The strength of these cycles is seen to vary over time, fading in and out over the millennia. The variation in the sun’s brightness over these longer cycles may be many times greater in magnitude than that measured over the short Schwabe cycle and so are seen to impact marine productivity even more significantly.

Our finding of a direct correlation between variations in the brightness of the sun and earthly climate indicators (called proxies) is not unique. Hundreds of other studies, using proxies from tree rings in Russia’s Kola Peninsula to water levels of the Nile, show exactly the same thing: The sun appears to drive climate change.

However, there was a problem. Despite this clear and repeated correlation, the measured variations in incoming solar energy were, on their own, not sufficient to cause the climate changes we have observed in our proxies. In addition, even though the sun is brighter now than at any time in the past 8,000 years, the increase in direct solar input is not calculated to be sufficient to cause the past century’s modest warming on its own. There had to be an amplifier of some sort for the sun to be a primary driver of climate change.

Indeed, that is precisely what has been discovered. In a series of groundbreaking scientific papers starting in 2002, Veizer, Shaviv, Carslaw, and most recently Svensmark et al., have collectively demonstrated that as the output of the sun varies, and with it, our star’s protective solar wind, varying amounts of galactic cosmic rays from deep space are able to enter our solar system and penetrate the Earth’s atmosphere. These cosmic rays enhance cloud formation which, overall, has a cooling effect on the planet. When the sun’s energy output is greater, not only does the Earth warm slightly due to direct solar heating, but the stronger solar wind generated during these high sun periods blocks many of the cosmic rays from entering our atmosphere. Cloud cover decreases and the Earth warms still more.

The opposite occurs when the sun is less bright. More cosmic rays are able to get through to Earth’s atmosphere, more clouds form, and the planet cools more than would otherwise be the case due to direct solar effects alone. This is precisely what happened from the middle of the 17th century into the early 18th century, when the solar energy input to our atmosphere, as indicated by the number of sunspots, was at a minimum and the planet was stuck in the Little Ice Age. These new findings suggest that changes in the output of the sun caused the most recent climate change. By comparison, CO2 variations show little correlation with our planet’s climate on long, medium and even short time scales.

In some fields the science is indeed settled. For example, plate tectonics, once highly controversial, is now so well-established that we rarely see papers on the subject at all. But the science of global climate change is still in its infancy, with many thousands of papers published every year. In a 2003 poll conducted by German environmental researchers Dennis Bray and Hans von Storch, two-thirds of more than 530 climate scientists from 27 countries surveyed did not believe that the current state of scientific knowledge is developed well enough to allow for a reasonable assessment of the effects of greenhouse gases. About half of those polled stated that the science of climate change was not sufficiently settled to pass the issue over to policymakers at all.

Solar scientists predict that, by 2020, the sun will be starting into its weakest Schwabe solar cycle of the past two centuries, likely leading to unusually cool conditions on Earth. Beginning to plan for adaptation to such a cool period, one which may continue well beyond one 11-year cycle, as did the Little Ice Age, should be a priority for governments. It is global cooling, not warming, that is the major climate threat to the world, especially Canada. As a country at the northern limit to agriculture in the world, it would take very little cooling to destroy much of our food crops, while a warming would only require that we adopt farming techniques practiced to the south of us.

Meantime, we need to continue research into this, the most complex field of science ever tackled, and immediately halt wasted expenditures on the King Canute-like task of stopping climate change.

http://www.canada.com/nationalpost/financialpost/comment/story.html?id=597d0677-2a05-47b4-b34f-b84068db11f4p=4

Jack

Kentucky or Texas? Which do you like better? Why?

Monday, April 27th, 2009
Which state do you prefer? Why? Ever lived in or visited them?

I live in KY but much prefer TX. I think TX has more to offer in terms of arts, culture, diversity in natural beauty, and history. Plus, I think its people are much friendlier.

I’m sorry if I offend any Kentuckians, but that is my personal experience. However, while KY doesn’t have as much DIVERSITY in natural vegetation and topography as TX, I think it’s still prettier than TX. From the lakes and returned-to-nature lands of west KY to the rolling bluegrass around Lexington to the mountains of east KY, it’s really a pretty state.

Norene

I don’t understand this Geology question. Please help?

Sunday, April 26th, 2009
In the U.S. topography maps commonly cover areas that include 7 1/2′ of longitude by 7 1/2′ of latitude or 15′ of longitude by 15′ of latitude. Such maps are commonly called 7 1/2′ of minute or 15′ minute maps (quadrangles) respectively. Usual scales used for topographic maps in the U.S. are 1:24,000 and 1:62,500.

Why do 7-1/2′ quadrangles in Arizona contain more square miles of area than 7-1/2′ quadrangles in North Dakota?

Can someone explain what I need to do?

Rosario

Help with writing a thesis?

Sunday, April 26th, 2009
I need a good thesis for my essay on the culture/beauty/topography of South Africa.

can anyone of you guys help? =].

Tinisha

Where can i find this info?

Thursday, April 23rd, 2009
i have my geoscience class and i need to know something about this climate called ARID…
*Typical latitudes.
*Topography.
*Proximity to water.
*Global Winds Patterns(if they converge or differ)..
Please HELP!!!!!!

Ninfa

Problems in north asia?

Wednesday, April 22nd, 2009
Guys can you give me 5 countries in north Asia with 3 categories of PROBLEMS each?
1. Values and attitude of the people.
2. Lack of technical knowledge
3. Corruption of the government
4. Topography and landform
5. Climate

Gabriele

Help with these science questions? 6th grade?

Friday, April 17th, 2009
15. All of the water on Earth is contained in me. I am mostly made up of salt water from the oceans, but I also contain fresh water. What am I?

16. I am not a sphere. I am a source of energy for processes on Earth. What am I?

17. I am the outermost sphere. I am a mixture of gases that surrounds the planet. I am mostly made up of nitrogen and oxygen. What am I?

18. I am Earth’s solid rocky outer layer. All of Earth’s continents and islands are on me. I also make up the ocean floor. What am I?

19. Name the ways energy can be transferred. Give an example of each.

20. What three factors does topography of an area depend on?

22. Latitude lines run ____________ of the equator. The equator cuts the Earth into the __________ and __________ hemispheres. Longitude lines circle the globe from the _______ to the ____________. Zero degrees longitude is known as the ___________ and _________ hemispheres.

23. Why are latitude lines lines considered parallels and longitude lines are not?

24. What city does the Prime Meridian run thorough in the Northern Hemisphere?

26. Fill in the blanks below.

LANDFORM ELEVATION RELIEF
Plains Low or high ______
_______ High High
_______ High Low

27. Match each term with its definition by writing the letter of the correct definition on the line beside the term.

TERMS
27. latitude
28. plateau
29. topography
31. elevation
32. relief
33. landform region
34. plain
35. longitude

DEFINITION

a. the height above sea level of a point on Earth’s surface
b. the shape of the land
c. flat or gently rolling land with low relief
d. a large area of land for which the topography is mainly one type of landform
e. the distance in degrees north or south of the equator
f. the distance in degrees east or west of the prime meridian
g. the difference in elevation between the highest and lowest points of an area
h. a landform that has high elevation and a more less level surface

37. A(n) __________ map shows the surface features of an area

38. The change in elevation from one contour line to the next is called the _____________

39. A(n) ____________ connects points of equal elevation on a topographic map

I’m not a lazy kid seeking answers. I had a bad day in school I returned from being sick and I left my science book in my locker. Please help! can you help me?

Cammy

GREEK HISTORY 10 POINTS?

Thursday, April 16th, 2009
hey im doing a assignemnt i need to know the physical geography, climate, topography and natural resources, and population thanx:)
as i am having trouble finding info

Leonida

Mapping Earth surfaces 3. Please help?

Thursday, April 16th, 2009
11. What do geologist call an area where there is mostly one kind of topography?

12. What is a mountain range?

13. Compare the elevation of a coastal plain to that of an interior plain?

14. The south Island of New Zealand lies at about 170 degrees E. What hemisphere is it in?

15. Could countour lines on a map ever cross?

16. Wich would be more likely to show a shallow, 1.5-meter-deep depression in the ground: a 1 meter countour interval or a 5- meter countor interval. Explain

Monique

earth science helpppp?

Wednesday, April 15th, 2009
okay so i was out for two days and i have so much earth science hw plz help me with ittt do the ones u know plz

1) why would you expect to find disorted rock structures in mountain landscapes?

2) the major landscape regions of the united states are identified chiefly on the basis of
1. similar surface characteristics
2. similar climatic conditions
3. nearness to major mountain regions
4. nearness to continental boundaries

3) in which new york state landscape region is 44 N latitude and 74,30 W longitude found?
1. hudson-mohawk lowlands
2. st. lawrence lowlands
3. adirondack mountains
4. the catskills

4) whicn new york state landscape region has the lowest elevation, the most level land surface, and its composed primarily of cretaceous through pleistocene unconsolidated sediments?
1. the hudson-mohawk lowlands
2. the atlantic costal plain
3. the champlain lowlands
4. the erie- ontario lowlands

5) boundaries between landscape regions in new york state are best described as being
1. straight lines running north and south
2. invisible on the surface
3. usually well defined
4. generally unchanging

6) the boundaries between landscape regions are usually indicated by sharp changes in
1. bedrock structure and elevation
2. weathering rate and method of deposition
3. soil associations and geologic age
4. stream discharge rate and direction of flow

no number 7
8) the adirondacks and the catskills are both areas of high elevation. why are the adirondacks classified as a mountain landscape, whereas the catskills are classified as a plateau landscape?

9) landscape regions in which leveling forces are dominant over uplifting forces are often characterized by
1, valcanoes
2. mountain building
3. low elevations and gentle slopes
4. high elevations and steep slopes

10) in a certain area the processes of uplift and leveling are in dynamic equilibrium. if this condition continues, what will be the over all long term effect on the elevation of the area?

11) which chnage would occur in a landscape region where uplifting forces are dominant over leveling forces?
1. topographic features becoming smottther with time
2. no dynamic equilibrium over time
3. streans decreasing in veloctiy with time
4. hillslopes increasing in steepness with time

12) which characteristics of a landscape region would provide the best information about the stage of development of the landscape?
1. the age and fossil content of the bedrock
2. the types of hillslopes and the stream patterns
3. the amount of precipitation and the potential evapotranspiration
4. the type of vegetatin and the vegatation growth rate

13) which factor is most important in determining the evolution of a landscape?
1. surface topography
2. plant cover
3. climate
4. develpoment of drainage

14) list two landscape characteristics you would expect to find in an area which has undergone glacial erosion.

15) contrast the cross sectional profiles of a glacial valley and a stream valley.

17. characteristics such as composition, porosity, permeability, and particle size are usually used to describe different types of
1. hillslopes
2. stream drainage patterns
3. soils
4. ridges
the point is i ll hand in my homework and get credit for it
idc about understanging cuz i know i wont understand it.
yes i expect to get credit for something i didnt do. nd no i wont tell my teacher to change it cuz its from a textbook. but reading the pages doesnt help u answer the question. its not like english. so there fore i dont want to do it. thanks for ur helppppppppppppp though.

Julene