Air Masses

An air mass is a large body of air that has similar temperature and moisture properties throughout. The best source regions for air masses are large flat areas where air can be stagnant long enough to take on the characteristics of the surface below. Air masses are defined according to both their region of origin and their course travelled. The main types include maritime tropical (mT), maritime polar (mP), maritime Arctic (mA), continental polar (cP) and continental tropical (cT) air masses. These descriptions are used both in the Britain and Europe, and in the United States. The maritime Arctic (mA) air mass, for example, originates in the Arctic and travels across the relatively warm stretch of the North Sea to affect the climates of northern Europe. Maritime tropical air (mT), on the other hand, originates near the Gulf of Mexico and travels north-east across the warm Atlantic to affect western Europe, as well as north-west across the United States. In Europe, continental polar air comes from Siberia, whilst in North America, it originates over the northern plains of Canada.

As a general rule, maritime air masses are generally fairly moist, containing considerable amounts of water vapour, which is ultimately condensed and released as rain or snow. By contrast, continental air is usually a lot drier. Once an air mass moves out of its source region, it may be modified as it encounters surface conditions different to those found in the source region. For example, as polar air moves southward, it encounters warmer land masses that heat it by the ground below. Polar and tropical air masses typically clash in the middle latitudes, producing some very changeable climates, typically experienced in the British Isles.

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The Black and White Aerosols Show

A paper published in Nature Geoscience last month received a lot of media attention. And rightly so. It showed that the Black Carbon (BC) component of soot is responsible for up to 60% as much warming as CO2. That is significant for many reasons, only some of which were covered in the newspapers.

The Guardian’s account is fairly typical:

Scientists warn of soot effect on climate

· Coal and wood ‘more damaging than thought’

· Black carbon harms environment and health

Most reports also mentioned that BC-induced warming is more amenable to mitigation than that caused by CO2. This is because BC persists in the atmosphere for periods of days rather than the decades that CO2 does, so reductions in BC output will take more immediate effect, and because BC and the so-called white aerosols such as sulphates, which have a cooling effect, have only partially overlapping sources, providing the potential to decouple white and black aerosol production. So far, so interesting. But what didn’t get mentioned is even more so.

First, there are the implications of the research for the climate models. It hardly needs pointing out that the identification of a factor that causes 60% as much warming as CO2 is going to require something of a re-adjustment of the models. The graph that usually gets wheeled out on such occasions is this one, which shows how the models juggle what are thought to be the five major forcing factors to come up with a line that kind of agrees with observed temperature variation over the last century:

Black carbon doesn’t even feature. In its latest round of reports, the IPCC assigns BC a warming effect of 0.2-0.4 Wm-2 (a consensus figure based on 20-30 modelling studies), in contrast to the Nature Geoscience paper’s estimate of 0.9 Wm-2 (the result of a review of the models combined with new empirical data from satellites, as well as aerial and terrestrial measurements of “brown clouds” over the Indian Ocean and Arabian Sea).

More generally, the findings reveal how little is understood about the role of aerosols (regarded as having a net cooling effect) on climate dynamics. Which is especially interesting because aerosols are absolutely central to the standard way of explaining away a thorny problem for global warmers – the period of cooling (~1944-1974), which occurred in defiance of rising CO2 concentrations (see graph above). The argument goes that the temperature slump is the result of white aerosols – released from coal and oil burning – masking the warming effect of anthropogenic greenhouse gases, until various clean air acts in the US and Europe allowed the anthropogenic warming signal to re-emerge.

Indeed, this is one of those items of ‘settled science’ flagged up in an open letter to Martin Durkin’s Wag TV, makers of the infamous The Great Global Warming Swindle, organised by Bob Ward, former Senior Manager for Policy Communication at the Royal Society and now Director of Global Science Networks at risk analysis firm RMS and signed by 37 scientists. The letter demanded that Wag TV correct “five major misrepresentations of the scientific evidence” before distributing the DVD version of the program. One of those major misrepresentations concerned the post-war temperature slump:

However, the DVD version of the programme does not make any mention of the impact of atmospheric aerosols on the record of global average temperature. The producer of the programme, Martin Durkin has attempted to justify this by suggesting that if aerosols caused the cooling between 1945 and 1975, then global average temperatures should be lower today, because he believes that atmospheric concentrations of aerosols should be even higher today than they were during that period. But the IPCC Fourth Assessment Report pointed out that “[g]lobal sulphur emissions (and thus sulphate aerosol forcing) appear to have decreased after 1980”.

However, according to the authors of the Nature Geoscience paper, it is nothing like so clear cut. First up, University of Iowa atmospheric chemist Greg Carmichael:

Climate Resistance: Are we now not so certain that the post-war cooling is due to aerosols?

Greg Carmichael: This is an added complication. But it’s also an added level of understanding. And as we get better measurements of the present, and better models that can drive these simulations for the last 50 years, or so, we’ll see that we’ve improved our understanding and that the aerosol effect is as important as we’ve indicated.

CR: But we don’t actually know that yet?

GC: We still have a way to go before understand how the heating-cooling push-pull really plays out.

UC San Diego atmospheric physicist Veerabhadran Ramanathan is more candid:

Climate Resistance: What are the implications of this work for the idea that the post-war temperature decline is the result of sulphate aerosols masking the warming effect of CO2 emissions?

Veerabhadran Ramanathan: After the 1970s, when the West was cleaning up pollution, there was a rise in temperatures. We stopped burning coal in cities etc, and coal puts out a lot of sulphates, and sulphates mask global warming. At the same time, in the tropics, China and India, they were growing fast and putting a lot more Black Carbon.

CR: So the sulphate component must have been reduced more than the Black Carbon component for the aerosol masking theory to hold? We now need empirical data to compare the effect of black and white aerosols during the post-war temperature slump?

VR: Exactly.

CR: Do we have that empirical data?

VR: No. The data we have is for 2002-2003. We don’t know what happened in the ’50s, ’60s and ’70s. The implication of this study is that we have to understand what is the relative change in the sulphur emissions versus the Black Carbon emissions – and we don’t know that.

CR: So what is the empirical evidence that, 50 years ago, white aerosols were masking GW due to CO2?

VR: It’s pretty flimsy. The main information we have […] is our understanding of the SO2 emissions by coal combustion, and oil. But we need to know not so much how much SO2 we put out, but how much was converted to sulphates, how much was removed [etc]

CR: So you don’t even know the life cycle of the SO2 and sulphates?

VR: No. All the information we have is from models… It could still be true [that white aerosols account for the post-war temperature slump]

CR: But it could not be true?

VR: Yes. The picture is complicated. But this paper is not saying it is wrong […]

CR: So we now have a better idea of what is happening aerosol-wise in the present, but what was going on in the 1950s/’60s is still elusive?

VR: Yes, There’s a lot of research needs to be done on that – what happened in the ’50s and ’60s, and then why the rapid ramp up [from the ’70s]. I’m not saying our current understanding is wrong, just that it is a more complicated picture. I would say it’s uncertain.

All of which tells a rather different story about the state of knowledge than Bob Ward’s letter would have us believe. It continues:

[The Great Global Warming Swindle] misrepresented the current state of scientific knowledge by failing to mention that the cooling effects of aerosol need to be taken into account when considering the period of slight cooling between 1945 and 1975.

Just like Bob Ward failing to mention that the empirical evidence that aerosols account for the period of slight cooling between 1945 is “pretty flimsy”, in fact – which is perhaps why Durkin didn’t mention it. And just as Ward slights Durkin for bolstering his case by omitting ‘inconvenient’ facts, there is little difference between what he accuses Durkin of, and the way he and his fellow accusers carried on.

source:http://www.climate-resistance.org

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Forest Fires

Each year, fires burn millions of hectares of forest worldwide.

The resulting loss and degradation of forested land is roughly equal to that caused by destructive logging and conversion to agriculture combined, and has wide-reaching consequences on biodiversity, health and the economy, among others.

Fires good and bad
Fire is sometimes essential for forest regeneration, or provides tangible benefits for local communities. In other cases it destroys forests and has dire social and economic consequences.

Forest fires are a natural part of ecosystems in many, but not all, forest types: in boreal and dry tropical forests for example they are a frequent and expected feature, while in tropical moist forests they would naturally be absent or at least rare enough to play a negligible role in ecology.

When fires become a problem…
Fires become a problem when they burn in the wrong places, or in the right places but at the wrong frequency or the wrong temperatures. Fires in forests that burn under natural circumstances become a problem when those forests are used for a particular purpose, such as settlement or timber production.

Pervasive human influence
Globally, most forest fires are probably now directly or indirectly influenced by humans. But in many areas that are hot and dry for part of each year, where frequent fires would be expected, human influence has now become so pervasive that most fires are ‘unnatural’.

Fires in a flux
Objectives and aims of fire management are not synchronized or thought-through, leading to unwanted and wanted fires, which can result in both beneficial and damaging effects. The geographical spread, frequency and intensity of fires are all changing.

Fire is also used as a management tool because it is cheap, simple to apply (particularly important if use is illegal) and sometimes the only option available for poorer people and smallholders.

Underlying factors
Fires are usually signs of bigger, underlying problems. These underlying problems or factors include inappropriate economic incentives (such as subsidies for plantation agriculture) that stimulate the use of fire as a means of clearing forested land, inequitable or unclear land tenure leading to land and resource conflicts, failure to recognize or respect customary law, and weak or under-resourced government institutions.

Devastating to forests & humans
The immediate impact of forest fires can be devastating to human communities and forest ecosystems alike.

Fires can alter the structure and composition of forests, opening up areas to invasion by fast-colonizing alien species and threaten biological diversity.

Buildings, crops and plantations are destroyed and lives can be lost. For companies, fire can mean the destruction of assets; for communities, besides loss of an important resource base, fire can also lead to environmental degradation through impacts on water cycles, soil fertility and biodiversity; and for farmers, fire may mean the loss of crops or even livelihoods.

Health hazards
Severe forest fires, such as those in Indonesia in 1997/1998 and in Australia in 2001/2002, bring critical and in some cases life-threatening levels of pollutants. The health of as many as 75 million people may have been adversely affected by the Indonesian fires, with some 40,000 hospitalized for respiratory and other pollution-related ailments such as asthma, bronchitis and pneumonia, as well as eye and skin problems. The total cost of the fires was estimated at US$9.3 billion.

At the moment, action to combat forest fires only takes place when fires are burning, with rare attempts made to address the underlying causes.

Importance of local communities
Since government capacity is often lacking at local level, local communities are becoming increasingly involved in forest management and conservation, to the extent that many governments now expect communities to participate in managing fires.

 

source:http://www.panda.org

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Geothermal Energy:How It Works

The centre of the Earth is around 6000 degrees Celsius – hot enough to melt rock. Even a few kilometres down, the temperature can be over 250 degrees Celsius.

In general, the temperature rises one degree Celsius for every 36 metres you go down.

In volcanic areas, molten rock can be very close to the surface.Geothermal energy has been used for thousands of years in some countries for cooking and heating.

The name “geothermal” comes from two Greek words: “geo” means “Earth” and “thermal” means “heat”.

How it works

Hot rocks underground heat water to produce steam.
We drill holes down to the hot region, steam comes up, is purified and used to drive turbines, which drive electric generators.

There may be natural “groundwater” in the hot rocks anyway, or we may need to drill more holes and pump water down to them.

a geothermal power station

The first geothermal power station was built at Landrello, in Italy, and the second was at Wairekei in New Zealand. Others are in Iceland, Japan, the Philippines and the United States.

In Iceland, geothermal heat is used to heat houses as well as for generating electricity.

If the rocks aren’t hot enough to produce steam we can sometimes still use the energy – the Town Hall in Southampton, England, is partly heated this way.

Southampton town hall

More details

Geothermal energy is an important resource in volcanically active places such as Iceland and New Zealand.
How useful it is depends on how hot the water gets. This depends on how hot the rocks were to start with, and how much water we pump down to them.

Water is pumped down an “injection well”, filters through the cracks in the rocks in the hot region, and comes back up the “recovery well” under pressure. It “flashes” into steam when it reaches the surface.

The steam may be used to drive a turbogenerator, or passed through a heat exchanger to heat water to warm houses. A town in Iceland is heated this way.

The steam must be purified before it is used to drive a turbine, or the turbine blades will get “furred up” like your kettle and be ruined.

See Also:

Find out more from Mighty River Power, New Zealand

A geothermal project in Hawaii http://www.geothermalhawaii.com/

A diagram showing a geothermal project http://www.geothermal.marin.org/GEOpresentation/sld037.htm


Advantages

  • Geothermal energy does not produce any pollution, and does not contribute to the greenhouse effect.

  • The power stations do not take up much room, so there is not much impact on the environment.

  • No fuel is needed.

  • Once you’ve built a geothermal power station, the energy is almost free.
    It may need a little energy to run a pump, but this can be taken from the energy being generated.

Disadvantages

  • The big problem is that there are not many places where you can build a geothermal power station.
    You need hot rocks of a suitable type, at a depth where we can drill down to them.
    The type of rock above is also important, it must be of a type that we can easily drill through.

  • Sometimes a geothermal site may “run out of steam”, perhaps for decades.

  • Hazardous gases and minerals may come up from underground, and can be difficult to safely dispose of.

Is it renewable?

Geothermal energy is renewable.
The energy keeps on coming, as long as we don’t pump too much cold water down and cool the rocks too much.

source:http://home.clara.net

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