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The Earth Story

@earthstory / earthstory.tumblr.com

This is the blog homepage of the Facebook group "The Earth Story" (Click here to visit our Facebook group). “The Earth Story” are group of volunteers with backgrounds throughout the Earth Sciences. We cover all Earth sciences - oceanography, climatology, geology, geophysics and much, much more. Our articles combine the latest research, stunning photography, and basic knowledge of geosciences, and are written for everyone!
We hope you find us to be a unique home for learning about the Earth sciences, and we hope you enjoy!
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Namib Naukluft National Park

The largest national park on the African continent and the fourth largest on Earth (covering an area larger than Switzerland) seems like a barren place, but despite appearances an ecosystem thrives in the harsh and dry environment, including reptiles, insects, hyenas, gembocks, bush elephants, mountain zebra, leopards and jackals. The giant dunes (including the tallest on the planet some 300 metres high) and desert landscapes of the Sossusvlei part of the preserve are also the country's main tourist attraction. There is hardly any rain here, some 10cm a year concentrated between February and April...most of the region's moisture comes from condensation in the form of fogs and mists arising from the cold Atlantic offshore.

It encompasses several types of landscape, including a chunk of the Namib, thought to be the oldest desert on Earth (having been arid for somewhere between 55 and 80 million years, and visible as the orange area in the middle of the photo), along with part of the Naukluft mountain range towards the top, a remnant of an ancient continental collision that occurred between 700 and 550 million years ago. The rocks consist of highly folded marine sediments (magnesian limestones, quartzites and shales), part of a nappe, a feature named after the French for tablecloth, and denoting a large block of crust that has detached from the continental keel and been overthrust onto other rocks during a continental collision.

The fog arises from an encounter between the cold upwelling Benguela current and the descending hot and dry limb of a Hadley cell (the cause of the globe's bands of deserts at similar latitudes north and south, see http://bit.ly/1rGO3Br and links therein). These fogs were once the terror of sailors, sometimes covering coast and desert for half the days in the year, and the entire stretch was once known as the skeleton coast, because if you were wrecked there, you were nearly certain to die there.

The mist is then carried ashore by winds, and the moisture that it carries is responsible for the brilliant colours of the sands as it oxidises the iron into a variety of yellow-orange-red hues. The same winds sculpt and shift the sand around in the erg (sand sea) into dunes. The older the dune, the stronger its colour.

Loz

Image credit: NASA

Source: facebook.com
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Why are high level clouds shifting polewards?

For the last several decades as global warming started to bite, the new trend listed in the title was noted in satellite data, leading to a debate as to the contributions of different drivers that may have brought about the phenomenon. Since the global distribution of cloud cover strongly affects local climates (as they reflect heat back towards space (if present) or allow the land/sea below to absorb more heat (if absent)), any change may bring about strong localised effects. Understanding the causes of this effect is important for understanding and future modelling of the effects of clouds in a changing climate, one of the less well understood areas and a current hot topic of research.

The two main contenders are radically different in their implications, though both are linked to the current warming. The previous favourite was that shifting jetstreams and the changes in surface weather patterns that they engender (see http://bit.ly/1T02BGu) were moving polewards pushing the 5-10 mile altitude clouds before them away from the mid latitudes. A new paper based on analysing 30 years of satellite data combined with a detailed computer recreation of air currents during this period suggests that the second main contender is the more likely driver: an expansion of the globe's tropical zones.

These major climatic zones (equatorial, tropical temperate and arctic) are linked to three great rising and falling gyres of air that redistributes heat and moisture from the most insolated area around the eqquator to the least at the poles (see http://bit.ly/1VR8tUY for more detail, illustrated by a volcanic plume meeting a cell boundary). Hot air rises in equatorial zones foor example, dumps its rain and drops again bone dry in the subtropics, creating a global belt of deserts in both hemispheres. As the world warms the sinking branches of the calls are moving towards each pole, bringing changes in local weather patterns behind it. Tropical air currents meet the high altitude clouds as the branch migrates and push them towards the apices of Earth's rotation.

Loz

Image credit: NASA

http://go.nasa.gov/23xPOwA Original paper, paywall access: http://bit.ly/273nXJb

Source: facebook.com
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Have you ever questioned “why are hot deserts found along the tropics and not at the equator where the suns ray are most intense?" Question no more!  The reason for this is due to an Atmospheric Circulatory system known as “The Hadley Cell”. The Hadley Cell is essentially a thermal loop and is located between 30 degrees north and south of the equator. It works on the basis of convection, in that warm air rises and cool air sinks. It can be broken into 5 stages as follows: 1. Due to the angle of incidence of the earth, the sun warms the equator intensely; as a result, the air is warmed and is forced to rise. 2. The air rises about 15km until it reaches the tropopause, at which stage a temperature inversion occurs and the air is forced to move north and south. 3. As the air moves North and South it has lost much of its latent heat and subsequently its moisture.  4. The now cool dry air starts to sink at around 30 degrees north and south of the equator and this is why the hot deserts can be found at these latitudes.  5. Finally to complete the loop, the cool dry air moves in to replace the warm moist air that is rising at the equator and is reheated and the cycle forms again. -Jean  More information: http://www.windows2universe.org/earth/Atmosphere/hadley_cell.htmlhttp://www.windows2universe.org/earth/Atmosphere/hadley_cell.html

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Seriously, what the ****

Ok, this page is called the Earth Story and we wouldn’t be true to our name if we didn’t post something on the major Earth Story impacting most of our readership…the fact that it’s cold as **** (pick whichever 4 letter word you feel is appropriate) in much of the United States.

The Earth’s climate is driven by one basic fact – the tropics receive more energy from the sun than the poles because the planet is a sphere and the poles angle away from the sun. On a simple planet that did not rotate but had an atmosphere, this setup would cause 2 convection cells to form. Air would rise at the equator, move north and south, cool, and sink at the poles. Countering this flow, cold air from the poles would south towards the equator and be gradually heated until it rises.

This simple circulation pattern is known as a Hadley Cell model for the weather. It is what the Earth tries to do – a conveyor belt bringing excess heat from the equator to the poles where it can be radiated to space.

But Earth rotates. Consequently, air can’t simply head north and south – it gets deflected by the rotation of the Earth and the Coriolis Effect. The single cell pattern is broken up and instead generally forms 3 cells in each hemisphere – one near the equator, a central one, and a cell isolated near the pole, with air rising and sinking at the boundaries between the cells.

At the boundaries between these cells, as a consequence of both the differences in pressure and the Coriolis Effect, the winds are sped up into what we know as Jet Streams.

At the North Pole, the jet stream typically keeps the coldest air somewhat in place. Oh, it migrates north and south sometimes but generally, arctic air swirls to the north, somewhat isolated by that jet stream and the fact that it’s in a different circulating cell.

Except…on occasion, something happening in one cell can push into another cell. If, for example, a high pressure system forms in the center cell, it could push north so far as to knock the other cell out of the way. That’s what you’re seeing in this image and that’s the “polar vortex” you may hear about on the news.

Normally the polar vortex sits pretty happily up at the North Pole. Today, it’s been pushed into the United States. The location of the jet stream was bent to the north, in part driven by high pressure over the Pacific and western U.S. As a consequence, the jet stream was forced deep into the southeastern U.S., bringing the air from the arctic all the way down to the Gulf of Mexico.

Of course, there are obviously people laughing at the idea of climate change every time it gets this cold. The first obvious answer is that still ignores what is happening in the southern hemisphere, such as Australia, which is currently mired in another record-breaking heat wave.  

Meanwhile, even in a climate changed world, the Arctic will stay extremely cold. The mean average winter temperature in the Arctic is around -40°C (-40°F). So far, the average global temperature has only increased by 1°C; even if the Arctic winter temperature jumped by 10°C it would still be incredibly cold up there. But the science is actually more interesting than just that.

The jet streams are held roughly in place by the temperature differences between the cells – that’s why even in summer it stays pretty cold at the poles, warmer air just doesn't get up there. But, as we've seen over the past few years, the Arctic is one of the fastest-warming places on Earth, with the icecaps shrinking rapidly and the open ocean starting to heat up. That means the temperature difference between the cells is, to some extent, decreasing as the arctic heats up.

There was a recent paper published by Dr. Jennifer Francis from Rutgers University arguing that as a consequence of this change, it is becoming easier to push the jet stream around. If the jet streams are more easily buckled by high pressure systems, the end result could be that extreme events like this one, caused by extreme bends in the jet stream, could become more common.

That science is still work-in-progress, but it is definitely interesting and it provides a mechanism for the increase in “extreme weather events” that has been documented in many countries over the past decade.

So that’s the U.S. right now. Extremely cold because the cold air usually trapped in the Arctic was punched to the south by a high pressure system. The world hasn't suddenly cooled down, this extremely cold air usually just sits somewhere else. And from a climate change perspective, we don’t know if events like this will become more or less common with time, but even in a climate changed world, events like this are certainly possible.

 -JBB

 Image credit: Greg Laden/ECMWF

Australian heat wave post:

Read more:

http://www.wunderground.com/news/polar-vortex-plunge-science-behind-arctic-cold-outbreaks-20140106

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