IN A TIME OF UNIVERSAL DECEIT...TELLING THE TRUTH BECOMES A REVOLUTIONARY ACT

"Capitalism is the astounding belief that the most wicked of men will do the most wicked of things for the greatest good of everyone." John Maynard Keynes

" Labor is prior to, and independent of, capital; that, in fact, capital is the fruit of labor, and could never have existed if labor had not first existed. Labor is the superior of capital and deserves much the higher consideration" Abraham Lincoln

Monday, July 4, 2011

WILL THIS BE ENOUGH? [and] BACKYARD RAMBLING

                         WILL THIS BE ENOUGH?
to finally get some momentum and political pressure going in the industrialised nations to reign in fossil-fuel emissions, and prevent runaway warming and catastrophic sea level rises? http://www.commondreams.org/headline/2011/07/01-6

We here at the Alaska Progressive Review have for some time have been giving you our assessment of the current state of the global climate, and it's rapid process of change, due to the release of CO2 and Methane, from fossil fuel combustion. Mainly from the industrialised nations, the two biggest sources being now China, and the U.S.
 
 
Of course all of our assessments have been based on the current state of the science of climatology, meteorology, and atmospheric physics. Now, more "official" governmental scientists are speaking out, and this IS IMPORTANT! Unfortunately, you aren't seeing much of this in the U.S. corporate media, note that the following article comes from the U.K.-based Independent, a somewhat progressive newspaper.

Extreme Weather Link 'Can No Longer Be Ignored'

Scientists to end 20-year reluctance with study into global warming and exceptional weather events

by Steve Connor

Scientists are to end their 20-year reluctance to link climate change with extreme weather – the heavy storms, floods and droughts which often fill news bulletins – as part of a radical departure from a previous equivocal position that many now see as increasingly untenable.
In this April 19, 2011 file photo, smoke rises from an uncontrolled wildfire burning near Possum Kingdom, Texas. It was a spring to remember, with America pummeled by tornadoes, floods, wildfire, snowmelt, thunderstorms and drought. (AP Photo/LM Otero, File)
Climate researchers from Britain, the United States and other parts of the world have formed a new international alliance that aims to investigate exceptional weather events to see whether they can be attributable to global warming caused by greenhouse gas emissions.
They believe that it is no longer plausible merely to claim that extreme weather is “consistent” with climate change. Instead, they intend to assess each unusual event in terms of the probability that it has been exacerbated or even caused by the global temperature increase seen over the past century.

The move is likely to be highly controversial because the science of “climate attribution” is still in the early stages of development and so is likely to be pounced on by climate “skeptics” who question any link between industrial emissions of carbon dioxide and rises in global average temperatures.
In the past scientists have been extremely reluctant to link a single extreme weather event with climate change, arguing that the natural variability of the weather makes it virtually impossible to establish any definitive association other than a possible general consistency with what is expected from studies based on computer models.

However, a growing number of climate scientists are now prepared to adopt a far more aggressive posture, arguing that the climate has already changed enough for it to be affecting the probability of an extreme weather event, whether it is an intense hurricane, a major flood or a devastating drought.

“We’ve certainly moved beyond the point of saying that we can’t say anything about attributing extreme weather events to climate change,” said Peter Stott, a leading climate scientist at the Met Office Hadley Centre in Exeter.

“It’s very clear we’re in a changed climate now which means there’s more moisture in the atmosphere and the potential for stronger storms and heavier rainfall is clearly there.”

Kevin Trenberth, a distinguished senior scientist at the US National Center for Atmospheric Research (NCAR) in Boulder, Colorado, also believes the time has come to emphasize the link between extreme weather and the global climate in which it develops.

“The environment in which all storms form has changed owing to human activities, in particular it is warmer and more moist than it was 30 or 40 years ago,” Dr Trenberth said.

“We have this extra water vapor lurking around waiting for storms to develop and then there is more moisture as well as heat that is available for these storms [to form]. The models suggest it is going to get drier in the subtropics, wetter in the monsoon trough and wetter at higher latitudes. This is the pattern we're already seeing.”

The Met Office and NCAR have joined forces with other climate organizations, including the influential US National Oceanic and Atmospheric Organization (NOAA), to carry out detailed investigations of extreme weather events, such as the vast flooding in Pakistan last year, to see whether they can detect a climate change “signal” as a likely cause.

A group of their researchers has formed a coalition called the Attribution of Climate-Related Events which is preparing a report on the subject to be published later this year at a meeting of the World Climate Research Program in Denver. They hope in the future to assess each extreme weather phenomenon in terms of its probability of being linked with global warming and then to post the result on the internet.

“There is strong evidence if you look across the world that we are seeing an increase in heatwaves and floods and droughts and extreme rainfall and extreme temperatures,” Dr Stott said.

“The evidence is clear from looking at the observational records globally that extreme temperatures and extreme rainfall are changing. But you can’t jump from that and say that a specific event is straightforwardly attributable because we know that natural variability could have played a part.

“We’ve been developing the science to be increasingly more quantitative about the links and make more definitive statements about how the risk has changed. You look sensibly about these things by talking about changing risk, or changing probability of these events.”

Dr Stott had his colleagues have already carried out studies of the 2003 heatwave in Europe, in which up to 35,000 people died of heat-related illnesses, as well as the devastating UK floods in 2000 which cost £1.3bn in insurance claims and destroyed 10,000 homes following the wettest autumn in England and Wales since records began in 1766.

In both cases, the scientists found that the contribution of man-made greenhouse gases to global warming substantially increased the risk of such extreme events occurring. The group is also investigating the exceptional warm April in Britain this year, which was the warmest since central England records were kept in 1659 and 0.5C warmer on average than the previous warmest April.

Also this year, an unprecedented number of tornadoes across the southeastern US and the flooding of major rivers such as the Mississippi and Missouri led many people to question whether they were exacerbated by global warming. In the past scientists would have been reluctant to link single weather events such as these with climate change, but Dr Trenberth believes this is wrong.

“I will not say that you cannot link one event to these things. I will say instead that the environment in which all of these storms are developing has changed,” Dr Trenberth told The Independent.

“It’s not so much the instantaneous result of the greenhouse effect, it’s the memory of the system and the main memory is in the oceans and the oceans have warmed up substantially, at depth, and we can measure that. I will assert that every event has been changed by climate change and the main time we perceive it is when we find ourselves outside the realms of the previous natural variability, and because natural variability is so large this is why we don't notice it most of the time.

“When we have things that occur usually 4 per cent of the time start to occur 10 per cent of the time, that’s when we begin to notice. The main way we perceive climate change is in changes in the extremes, this is when we break records.”

A report by the insurance company Munich Re found that 2010 was one of the worst years on record for natural disasters, nine-tenths of which were related to extreme weather, such as the floods in Pakistan and eastern Australia and heatwave in Russia, which is estimated to have killed at least 56,000 people, making it the most deadly natural disaster in the country’s history.

“This long-term trend can no longer be explained by natural climate oscillations alone. No, the probability is that climate change is contributing to some of the warming of the world’s oceans,” said Peter Höppe, author of the Munich Re report.
 
Making the connection
Tornadoes, US, 2011 More than 220 people were killed by tornadoes and violent storms that ripped through south-eastern United States in April; 131 were killed in Alabama alone. Fifteen people died in Tuscaloosa and sections of the city were destroyed.
 
Heatwave, UK, 2011April was the warmest since 1659, when records in England began. Sun-lovers flocked to St Ives, above, but fears of drought were raised. Rainfall in the UK that month was only 52 per cent of the long-term average.

Drought, Brazil, 2005 The Amazon region suffered the worst drought in more than a century. The floodplains dried up and people were walking or using bicycles on areas where canoes and river boats had been the only means of transport.

Floods, USA, 2005 Katrina was one of the five deadliest hurricanes in the history of the US, and it caused the destruction of New Orleans when levees were overwhelmed. Some 90 per cent of residents of south-east Louisiana were evacuated.
The other day, we set out for a 30 KM "slow-pack" in our backyard, to some areas we've been in a few times this past winter. Namely, we wanted to finally ascend "The Ramp", which at 1598 metres (5240 ft.), had eluded us twice, for different reasons. Although it was a cool, cloudy day, the promise of rain the next day, meant we had to give it our all, when we could at least stay dry, even if we did have to ascend into the clouds at times. We're calling it "slow-pack", versus our usual fast-packs, because we did have to ascend the Ramp in the fog, very slowly, so as not to lose our way, and fall into trouble.

At the top of Ship Lake Pass, which took about three hours to hike into, we were already just about in the clouds. But the view to the east, of beautiful alpine Ship Lake, was not to be missed. It's not too difficult of a descent, down into the lake, and Ship Creek Valley, but we had more ascending to do.
The view to the north, of the Ship Creek Valley, was also well worth the trip, even on a cool, cloudy day. Here at the top of the pass, it was about 5C (41F), with a steady 30 kph (18-20 mph) breeze. I definitely had to put a hat and gloves on, when we stopped here for a breather and some water. But the Ramp beckoned, even through the top 300 metres were totally obscured in the fog. We slowly ascended up its steep slopes, clad in tundra, mixed in with large areas of loose scree/talus, which sometimes easily gave way with just a slight pressure of the feet. Requiring us to be very careful. We knew the way though, from our previous attempts, and also that the valley/bowl we came up, was right below us, and still beneath the clouds. When we reached the ridgeline of the Ramp's sharp sharktooth-like peak, we actually felt a little queasy and disoriented in the thick fog, with visibilities of 10 metres or less. Because as we looked down into the abyss on the north side of the ridgeline, with it's sheer 300+ metre drop, we couldn't see the bottom. Homer is almost 15 now, and he had no problem ascending with us on these steep slopes, for which we were very greatful. But we give him lots of exercise, in outings like this, good food, and attention, which keeps him thriving.
We just spent a few minutes in the fog at the top of the Ramp, hoping for some clearing. Once in awhile, a thin spot in the clouds would let more light in, but the visibility never did improve to more than 20 metres or so. It was a cool 2-3C up there (35-38F), with a stiff south breeze, rather chilly. So we slowly descended back down the gentler, but still steep, south face, back to the valley we came up in. We had lunch where the the trail that takes off from the Powerline trail, splits in two, one branch heading to the Ship Lake Pass, the other to Hidden Lake. We hadn't been to Hidden Lake before, so we needed to check it out. It was just 3 or 4 more KM up, and another 300 metres or so of elevation. There was one small lake first, about 2 KM in, but after a steep rise, on the other side, in a bowl, part of whose headwall is the Ramp, lies the jewel of Hidden Lake, a very apt name, as it can't be seen, until you are right on it.
We are quite sure that on a rare sunny day, this lake would have that beautiful pale blue alpine colour we greatly prize in our outings, as it means these lakes are completely clean, wild, and unspoiled by any human activity (and also very cold!). It was starting to sprinkle a bit after we got here, so we didn't spend much time. Had it been a warmer, sunny day, there is no doubt I would have gone for a swim in there, I'd sure like to some day. We descended back down to the trail junction, and then down to the Powerline Trail. We still wanted to head in to an area we haven't seen before, so just before we reached the trailhead, we decided to head up the Middle Fork Loop trail, which has a steep ascent up a ridge on the other side of the valley that the Powerline trail is in. It was raining lightly at this point, but we didn't care, as we just had another hour or two, before finishing. As we ascended this steep section of trail, we ran into a group of 15 teenagers with two adult chaperones, on a five-day pack-trip. These kids were from all over the World, the adults are part of a group that takes teens on trips like this to build leadership and outdoor skills. All the kids just loved Mattie and Homer, since most had never seen real sled dogs, and were very nice. I told them to expect alot of rain on their trip, but I'm sure they had a good time.
Our ascent brought us up to 1050 metre (3500 ft) Little False Point, which has a beautiful view of the Anchorage "Bowl" and Cook Inlet, in the evening sun. It was getting later in the evening and I didn't bring full dinners for Homer and Mattie, so we headed quickly back down after that, and to the trailhead, so I could rush them home in the short 15 minute drive back to the CFRC, for dinner. After all, in our 30 KM 8 1/2 hour backyard ramble, Mattie must have done at least double that, with all her running around, and Homer, probably 40-50 KM. This is why we live here, to be so fortunate to have this for our backyard. 

Wednesday, June 22, 2011

TWILIGHT AT ELEVEN

That's the earliest twilight now starts here on the longest day of the year, at 61N. Then staying twilight until around 230 am, after which, the sun peeks back up over the horizon. It being one of our most significant dates, here at the Alaska Progressive Review, with thousands of years of historical significance, in every culture, and on every continent. So we felt a need to be in a peaceful natural setting, and we have many staked out around here in Anchorage. For which we are very fortunate.
An easy place to get to, we really like, is just 45 minutes of running from our door, here at the CFRC, which we do 4-5 times a week. This was last late October. But now being the summer solstice, is completely different. The North Fork of Campbell Creek Canyon, which we run to most days in summer, off the Tank Road. But sometimes for quicker access, we drive up to the end of Basher Road and park there. Then head down the steep trail. Views of the higher country quickly come in, which are nice in the spaces between the thick boreal forest. This part of the trail is very steep and potentially treacherous in all seasons.
At the bottom of the steep section, in the heart of the North Fork of Campbell Creek canyon, there is a little rock bridge you can sit on and enjoy the rushing water sound and sensations. We even had to go in past our ankles, it was so inviting, after a long day of running  and hiking.
  Further up the canyon, it opens up into tall grass fields, as you gain elevation above 1500 feet. The weather up here gets progressively colder and harsher by this altitude, than down in the city below 500 feet. The real high country really teases us as we keep going up. These peaks are only around 5000 feet, but they are completely devoid of life, nothing grows on them, not even lichens or moss, it is so cold and harsh, at that altitude.
We kept going with our picnic dinner about another mile, this is about 1.5 miles in from Basher road. About another mile in, there was a nice log to sit on and enjoy dinner, that was just open enough to allow a breeze through, and keep the bugs down.
Mattie is completely on guard, with all her senses, when we stop in places like this. She treed a black bear an hour into our three hour run today, just took straight off after it. I couldn't stop her. She truly has the energy and courage of two dogs in that little body of hers. We trust her implicitly to warn us of and fend off any danger. Homer does his best too. He keeps watch on the trail downhill. For people or other animals coming up. He is an imposing presence, to be sure. But completely gentle, and mellow now in his old age. I've known him for ten years now, and he did exact a harsh discipline when he was in charge of a 34 dog kennel in Fairbanks. I knew then how special he was, and was so glad when he came to us two years ago. He has great wisdom on many things, in his advanced age of nearly 15. We had a nice dinner here this evening in the gentle evening light. Heading back, viewpoints like this offered very nice peaceful views looking back over parts of Anchorage, to Cook Inlet. Anchorage is in a very special and favored place between mountains and the sea, protected from the coldest interior air by the Alaska Range, and sheltered from the heaviest rains and strongest winds associated with Gulf of Alaska low pressure systems, by the Chugach Mountains all year.


After a cool and cloudy morning, with a few sprinkles, the gentle evening light in the sunshine was very welcome, on this longest day of the year. That's what it looks like here at 2200 hours at 61.15 North, in the sub-Arctic. Happy Solstice! It is much cooler here in summer, than in the Interior. to the north, so days like this, are really special. A nice time to reflect on the good things we have here. We have to take breaks from the reality we see, as dilineated here, http://blog.buzzflash.com/node/12787, and get out into the natural world. For energy, inspiration, and healing.

Tuesday, June 7, 2011

WE DREAM OF GINI

The GINI coefficient http://en.wikipedia.org/wiki/Gini_coefficient is a relative measure of income and "wealth" equality. It can, if interpreted judiciously, thinking about the structures and cultures of the countries being assessed, give an accurate picture of the relative health and stability of a nation, based on it's measured inequalities. 

In this case, if we just look at "industrialised" nations, the U.S. is quite low in the assessment, meaning the inequality in wealth, and income, is very high. Note that Mexico, and China, are now in the same grouping, as the U.S. However, remember, this is a relative index. But, in U.S. average income terms, which are much higher than those in Mexico, or China, our society is as unequal as theirs. Of course, in Mexico, and to a certain extent, China, the population of these nations as a whole, have less access to the things we accept as "normal", namely, clean safe tap water, wherever we are, proper sanitation, and a "safe" food supply, wherever we choose to obtain it. In addition most "poor" people in the U.S. have electricity (pre-supposing they are able to afford housing) and the ability to at least obtain food that will ensure their survival in a basic sense. 

However, these things are not to be taken for granted. If current trends and policies continue, the U.S. will develop the structure and insecurities of current "third world" nations within a decade or two.
Your lead editor has visited, lived in, and experienced other countries, where the GINI Index is much lower. And have felt that, as a whole, the majority of the people in these countries, feel happier, and are more satisfied with their nations, feel more a part of and connected to their neighbours and with how they fit in, their nation's role at large, in the World. Countries like Australia, and Canada, and of course, most of Western Europe. Why don't we learn from them, after all, most of us can trace our ancestries back to these countries, and still have connections with them. 

OK, here is a quick assessment of what I learned about Australia, when I stayed there for six weeks in 2008/09. It has a "social democracy" similar to the U.K., New Zealand, Canada, and most other western European countries. 

Minimum Wage: $15.38 per hour AUSD (exchange rate in 2008 with USD about .85)
Health Care: All citizens have universal insurance coverage. Complete health care is available to all. Similar to the U.K.
Vacation: All citizens receive at least four weeks leave, private or public sector.
Unemployment: $1543 AUSD per month. Unlimited, but they have strong, successful fraud monitoring, job application requirements, and job placement services.

Yet, something is different about the U.S., amongst all the industrialised nations. This chart tells a very big picture. Other than Singapore and Hong Kong, the U.S. is far and away the most inequal. And measures poorly in many other of these statistics. This is a direct result of the concerted political strategies of "conservative" politicians since the 1970s, but which really accelerated in the 1980s, and continue unabated to the present day.
We liked this article. http://www.commondreams.org/view/2011/06/05-1 It is written by a true psychologist, so someone who would be able to provide informed and unbiased assessments.

The Rise of the Second-String Psychopaths

The great writer Kurt Vonnegut titled his final book A Man without a Country. He was the man; the country was the United States of America. Vonnegut felt that his country had disappeared right under his – and the Constitution’s – feet, through what he called “the sleaziest, low-comedy Keystone Cops-style coup d’état imaginable.” He was talking about the Bush administration. Were Vonnegut still alive in the post-Bush era, he would not have felt that his country had returned.

How had our country disappeared? Vonnegut proposed that among the contributing factors was that it had been invaded – as if by the Martians – by people with a particularly frightening mental illness. People with this illness were termed psychopaths. (The term nowadays is anti-social personality disorder.) These are terms for people who are smart, personable, and engaging, but who have no consciences. They are not guided by a sense of right or wrong. They seem to be unaffected by the feelings of others, including feelings of distress caused by their actions. Straying from a decent way of treating people, or violating ethical codes causes no anxiety, the anxiety which is what causes the rest of us to moderate our more greedy impulses. If most children feel anxiety when they are pilfering the forbidden cookie jar, psychopaths feel just fine. They can devour the cookies, shatter the jar as evidence and stuff it in the trash can. When accused, they can argue with apparent sincerity that the cookie jar has been missing for at least a week. There suffer no remorse, no guilt, no shame. They are free to do anything, no matter how harmful.

Psychopaths can be very tricky to recognize. As psychiatrist Dr. Hervey Cleckly wrote in his classic The Mask of Sanity in 1941, psychopaths are not technically insane. They don’t have a psychosis, like schizophrenia. They are experts in appearing normal. They can act the role of a caring, concerned executive, even though they actually do not seem to experience such feelings. If they hurt somebody, they don’t modify their behavior.

The United States corporate and government spheres have become, Vonnegut suggested, a perfect habitat for psychopaths. What has allowed so many psychopaths to rise so high in corporations, and then government, he wrote,

“is that they are so decisive. They are going to do something every fuckin’ day and they are not afraid. Unlike normal people, they are never filled with doubts, for the simple reason that they don’t give a f..k what happens next. Simply can’t. Do this! Do that! Mobilize the reserves! Privatize the public schools! Attack Iraq! Cut health care! Tap everybody’s telephone! Cut taxes on the rich!
In a country in which much of human culture has been rendered into machines for the manufacture of money, psychopaths are the ideal leaders. They are very focused. They are outcome oriented. They are frequently charming, and usually very bright and able. They can lay off thousands of people, or deny people health care, or have them waterboarded, and it does not disturb their sleep. They can be impressively confident. Psychopaths can be dynamic leaders of enterprises, but are handicapped by their lack of feelings for relationships. They may be accomplished captains of industry, or senators, or surgeons, but their families are frequently abused and miserable. Most psychotherapists have seen the wives or husband or children of such accomplished people.


Since psychopaths are usually very smart, they can be quite competent at impersonating regular human beings in positions of power. Since they don’t care how their actions affect people, they can rise to great height in enterprises dealing with power and money. They can manufacture bombs or run hospitals. Whatever the undertaking, it is all the same to them. It’s just business.
The economic system that remains after the destruction of American local cultures has created an excellent employment picture for psychopaths. But the opportunities open to them are now so vast that there is apparently now an actual labor shortage. At least that is the only explanation I can find for the rise of a cadre of psychopathic leaders who resemble the usual type in all ways but one: they’re simply not that smart. One has only to look at right-wing not-so-Christian fundamentalists to see the peculiar emergence of a second-string of psychopaths.

The US has been endowed with abundant resources, and there have always been a more than sufficient supply of psychopaths of the first intellectual grade to supply corporate suites and their subsidiary, the Congress. Why is there now a downgrade to the dumb ones, like the lowering of standards for military recruits to deal with a shortage of cannon fodder?

It is no secret that the Koch brothers and others of the super-rich seem to have undertaken a final push to consolidate control through the conversion of a marginally democratic to an essentially fascist state; extreme right-wing, authoritarian, and demagogic. This kind of government is ideal for control of a populace by the moneyed elite. To carry this out requires the employment of many ‘kept’ politicians to excite and misdirect scared and angry – and ignorant – voters. Lest the citizenry realize who stole their money and storm their castles with torches, the rapacious elite need politicians who will carry out the work of re-directing anger at teachers, or labor unions, or the poor. I can only conclude that the people who now own the country couldn’t find any first-rate psychopaths to carry out their work. Or maybe the smart ones were all occupied. So they had to go to second-stringers, people who could actually believe what they were told to say.

We are a country who has become second-best, even in the quality of our psychopaths.
We at the Alaska Progressive Review, think that the reason so many people of this type are in charge of our political and economic system in the U.S. is because of the nation's unresolved and often suppressed racism. That is to say, a majority of the major ethnic group of it, European-descendants, are still afraid of other groups, African-Americans, Asians, Hispanics, and Native Americans. And that the "corporatocracy", or oligarchy, the major powers in U.S. society, the financial sector, fossil fuel, military-industrial, insurance, and other large corporate sectors, use this to persuade people to continue to vote against their own interests. How else can you explain Republican (and now even Democratic) politicians who would decimate social security and medicare, continue to grant tax benefits and breaks to the top few percent of the population and large corporations (that continually send more and more jobs to other countries, with U.S. government support) continuing to get re-elected? Of course, the corporate media does it's share to keep people uninformed, and that is a very large concern. Not to be ignored, and worthy of great concern.
But, the reason these other nations have benefits and security like they do, is because the people in them have more empathy, are not afraid of, and relate more, to their fellow people. A nation gets the government they deserve, in the sense that it is a reflection of the overall feelings and beliefs of the people in it. We think this idea is a good starting point for working for positive change. How do we really feel about people different from us? Of other cultures and ethnicities? Are all people equally worthy with respect to the culture we consider ourselves to be parts of? Are Indigenous peoples, who have completely different world-views, than most of ours in the U.S, culturally and spiritually "equal" to ours? Because if we don't think so, we'll never effectively solve global problems like overpopulation, resource depletion, environmental destruction, and global warming. Which if left unchecked will all combine to render a World much less inhabitable, for our descendants, within the next century. Cheers.

Friday, May 20, 2011

FAHRENHEIT 2051

or the temperature at which Anchorage burns? [apologies to Ray Bradbury, and Michael Moore, eds.]

What we are attempting to do in this article, is to quickly project what we think the climate of Anchorage will be fourty years hence, in the year 2051. Using the most up-to-date peer-reviewed scientific research. And your lead editor's 24 years of operational weather forecasting experience throughout the Western Lower 48 and Alaska. And no, we are not expecting Anchorage to burn up, necessarily, though fire seasons will certainly be a little longer, and more intense, than they are currently. But the Anchorage area, because of it's proximity to the cool waters of the Gulf of Alaska and Cook Inlet, will never have as extreme fire danger, or behaviour, as that seen further north, in the warmer (in summer), drier, interior. Your lead editor has some expertise in this area, having worked with and studied from some researchers at the University of Alaska, Fairbanks, and earlier, at the University of Montana, in Missoula. All involved on the cutting edge of climate change/global warming research.
Before projecting ahead though, we need to look at the current climate of the Anchorage area.

Anchorage is blessed with the most favourable climate for human habitation in the entire state! Perhaps that is why it is the largest population centre here. Why is that?
Well, let's look at some statistics, from the three main centres, in which we have all lived, since 1998. First, Juneau, which is a good representation for all of coastal Alaska, around the Gulf, from Kodiak to Ketchikan.
JUNEAU 2, ALASKA (504094)
Period of Record Monthly Climate Summary
Period of Record : 7/ 6/1965 to 12/22/2010
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Annual
Average Max. Temperature (F) 33.3 37.0 40.9 48.7 56.1 62.2 63.7 63.2 56.7 48.7 39.9 36.0 48.9
Average Min. Temperature (F) 24.5 27.3 30.3 34.9 41.5 47.9 51.0 49.9 45.3 38.9 30.8 27.2 37.5
Average Total Precipitation (in.) 6.96 6.12 5.98 5.01 5.67 4.23 5.75 7.57 11.93 12.87 9.45 8.54 90.08
Average Total SnowFall (in.) 24.2 12.0 7.7 0.8 0.0 0.0 0.0 0.0 0.0 0.3 8.0 15.8 68.8
Average Snow Depth (in.) 5 4 2 0 0 0 0 0 0 0 1 2 1

These numbers are from downtown Juneau, which is wetter, and milder, than the airport, or Mendenhall Valley, where the other large residential areas are. But 90 inches of precipitation (229 cm) is alot, and there is no real dry season, though April-July are "drier". Note how mild the winter temperatures are, and how short of duration the average snow depths are.



Because it is so close to the mild Gulf of Alaska, with usually some sort of flow off of it, it rarely stays well below freezing for periods of more than a week or two in winter, separated by rainy, milder, onshore flow periods. Which we found to our great dislike, as it meant good snow for nordic skiing would be ruined after a week or two. And running in driving rain at temperatures of 35-45F (1.5-8C) for much of the year, we found not to prefer. This sort of climate, can be found right around the corner, from Anchorage, up Turnagain Arm, in places like Girdwood, or Portage. Slightly colder and snowier in winter than Juneau, but still having rainy periods in winter disrupting good snow conditions, and much rainier in the warm season. So let's look at Anchorage's numbers:
This is the closest climate station to the Chugach Front Research Centre, about 5 KM to its west. So our winter temperatures are slightly colder than this, but summer's, about the same. And our precipitation is probably slightly higher, maybe by two to three inches (5 to 8 cm).
ALASKA PACIFIC UNIVERSITY, ALASKA (500172)
Period of Record Monthly Climate Summary
Period of Record : 7/ 1/1993 to 10/31/2004

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Annual
Average Max. Temperature (F) 21.0 28.5 34.4 46.3 56.9 64.9 67.5 65.5 56.6 41.3 28.9 23.5 44.6
Average Min. Temperature (F) 8.8 14.1 15.8 28.2 38.4 47.3 51.9 49.3 40.6 27.0 17.1 12.6 29.3
Average Total Precipitation (in.) 0.66 0.85 0.98 0.33 0.63 1.11 1.61 3.00 3.03 2.23 1.25 1.55 17.23
Average Total SnowFall (in.) 9.4 12.0 12.8 1.6 1.1 0.0 0.0 0.0 0.0 7.2 12.0 20.2 76.3
Average Snow Depth (in.) 13 14 17 6 0 0 0 0 0 2 6 11


Look at that annual precipitation, 17.23 inches (44 cm)! Versus the 90 inches (229 cm) in downtown Juneau! Note the colder winter temperatures, and deeper/longer average snow depths. This gives us one of the most favourable climates for nordic skiing, of any city on Earth! It's the Chugach Mountains, and the mountains on the Kenai Peninsula, which cup the Anchorage "bowl" from the northeast to the south, that work their magic for us. By protecting us from precipitation in east to south flows, which occur very frequently, as low pressure systems hang in the Gulf of Alaska for weeks on end, fed by the moisture and relative warmth (in the cool season) of the Pacific Ocean. Annual precipitation at the Alyeska Resort, near Girdwood, just 50 KM (31 miles) southeast, up Turnagain Arm, is 73 inches (185 cm). Note our increasing monthly precipitation values from May through September. In the weak summer jet stream, lows in the Gulf of Alaska become more frequent, and contain more moisture, as the summer wears into fall, and enough of their influence is felt here, but not nearly that seen just around the corner, or in Southeast Alaska, thank you Chugach Mountains!

The Chugach mountains also protect the Anchorage bowl from strong winds associated with other weather patterns as well. Just to the north, in the Matanuska and Susitna valleys, places like Palmer, Wasilla, and Talkeetna, have similar winter temperatures, but can receive very strong winds, especially from the Northeast and East, in the Matanuska valley, which are highly unpleasant in winter, and even scour all the snow away. Talkeetna, north in the Susitna valley, is wetter in summer, and hence boggier, with worse mosquito and fly densities.

What about further north, in Fairbanks? Well, these numbers tell the story very succinctly:

FAIRBANKS WSO AIRPORT, ALASKA (502968)
Period of Record Monthly Climate Summary
Period of Record : 9/ 1/1949 to 12/31/2010

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Annual
Average Max. Temperature (F) -1.2 8.4 23.7 42.6 60.1 70.8 72.3 66.3 54.7 32.2 11.6 1.5 36.9
Average Min. Temperature (F) -18.8 -14.0 -3.2 20.3 37.9 49.3 52.0 46.8 35.6 17.3 -4.8 -15.3 16.9
Average Total Precipitation (in.) 0.58 0.42 0.35 0.29 0.58 1.34 1.97 1.85 1.07 0.77 0.67 0.68 10.56
Average Total SnowFall (in.) 10.5 8.3 6.0 3.1 0.7 0.0 0.0 0.0 1.3 10.4 12.7 12.2 65.1
Average Snow Depth (in.) 17 21 20 10 0 0 0 0 0 2 8 13 7
Percent of possible observations for period of record.
Max. Temp.: 99.8% Min. Temp.: 99.8% Precipitation: 99.9% Snowfall: 99.9% Snow Depth: 99.8%

Those are quite cold temperatures, which represent the interior as a whole, from mid November through February. Sometimes much colder, and sometime warmer. Making outdoor recreation more cumbersome and less enjoyable, especially when combined with the shorter day and low light. It is drier in general, with sometimes very comfortable and enjoyable summers. But also much more prone to summer wildfires in the drier ones, which can lead to heavy smoke accumulations for long stretches, in very active seasons. Which are becoming more frequent.



So now that we have established that Anchorage's climate is the most benificent in the state, what kind of changes are likely in it, by 2051? We think it helps to first see how things have been changing over the past decades. http://climate.gi.alaska.edu/papers/Arctic62-3-295.pdf

We thought this table to be especially significant, showing the seasonal breakdown of temperature changes in each area of  the state. And that in the sixty years from 1949 to 2009, the average increase across the state has been +3F (+1.7C), more than the Earth, as a whole, but predicted by global climate modeling, the "Arctic Amplification". Driven by changes in duration of snow and sea ice cover, which change the "albedo" of the land/water. With shorter durations now of sea ice and snow cover, more solar heat is absorbed, for longer periods of the year.
Seeing how the seasonal breakdown of temperature increase has gone down for Anchorage, and surrounding areas, what does the latest climate change modeling suggest, for the next several decades?

This link, to the Arctic Climate Impact Assessment, research conducted and described by the most prominent atmospheric and climatic scientists in the World, projects, based on an average of the different global CO2 emissions scenarios, a global temperature increase of 2C by about 2050. Given that Alaska has already experienced twice the global increase over the past 60 years, we think it prudent then to expect a 4C average temperature increase across this area by 2051. But it won't be evenly spread across every month. We expect the 4C increase to generally follow the seasonal breakdown, that has already occurred over the past sixty years. Let's revisit that. The summer and fall increases are only half that of spring, and a quarter, of that of winter.

This makes sense, given the fact that we have noticed, over the past few decades, more "highly amplified" jet stream patterns of "meridional" flow, that is, flow more from south to north, than west to east, over Alaska and along the northwest section of North America, from about 40N, in winter and spring, when the jet stream is the strongest. Just a quick reminder, the jet stream is how heat is re-distributed to the poles, from the tropics. Because the poles lose more heat than they gain in solar energy, and the tropics gain more than they lose.

We're seeing more highly amplified patterns where large high pressure ridges extend much further north than they normally have been, in winter and spring. Moving tremendous masses of warm air aloft to very high latitudes, which eventually mixes down to the surface, over higher terrain, and along the north slopes of the Alaska Range, where very strong, dry chinook winds occur more frequently now, and which often produce high fire danger. So a continuance of this pattern is to be expected, and an amplification.
So let's re-work the Alaska Pacific University climate data, which is a proxy for what we see here at the Chugach Front Research Centre. Though our winter temperatures are somewhat colder, especially at night, due to our location in a slight depression, right at the front of the Chugach Range.

ALASKA PACIFIC UNIVERSITY, ALASKA (500172)
Period of Record Monthly Climate Summary
Period of Record : 7/ 1/1993 to 10/31/2051

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Annual
Average Max. Temperature (F)  30.0  36.7  42.3  52.4  58.6  70.0 69.0  68.5 61.0  47.4 34.5  30.4  50.0
Average Min. Temperature (F) 14.5  21.0  24.2  33.5  41.5  50.5  52.9  52.6  45.0 
34.2
 
24.4  18.3  34.3 
Average Total Precipitation (in.) 0.90 0.85 0.98 0.33 0.63 1.11 1.90 3.50 4.10  2.68 1.80 1.80 20.58 
Average Total SnowFall (in.) 18.9  15.0  10.3  0.5  0.0  0.0 0.0 0.0 0.0 2.4  15.0 29.3 91.4 
Average Snow Depth (in.) 18 16 12 0 0 0 0 0 13
Percent of possible observations for period of record.
Max. Temp.: 89.4% Min. Temp.: 89.4% Precipitation: 89.5% Snowfall: 89.1% Snow Depth: 87.7%
Check Station Metadata or Metadata graphics for more detail about data completeness.

The reason the summer increases are the lowest is due to Anchorage's geography.
As the interior, north of the Alaska Range, and in the Susitna Valley, just to the north of the Anchorage bowl, heats up more, overall in the summer, this pulls a south to southeast flow up through and around the region. Cool, maritime air, chilled by the waters of the Gulf of Alaska, Cook Inlet, and Turnagain Arm. Waters, which even in 2051, would only likely warm 1-2C by then, to around 10C in summer (50F). Still quite cool and able to keep average summer temperatures down. In fall, winter, and spring, more highly amplified high pressure ridging episodes would bring greater amounts of sub-tropical warmth for longer durations. Thus fall and winter snowfall would diminish, but in the depths of winter, increase. Snow cover would then take longer to establish in fall, and be earlier to melt, in Spring. By two to three weeks on each end. Winter extreme cold spells, where night-time temperatures can drop to -29 to -32C (-20 to -25F), would be more infrequent, and of shorter duration.

Let's look at a few specific hazards or problems that Anchorage faces, and how that would change.
Wind storms:
Most people have a general idea that the Gulf of Alaska and Bering Seas produce treacherous weather, in the form of deep low pressure systems, and strong fronts, especially from September through April. These don't strike Anchorage full-force, usually, because of our sheltered location, as mentioned before. But once in awhile, one can hold together with enough strength, in just the right pattern, to produce winds of 80-100 mph, or even stronger, along the hill-slopes of the Chugach Front. With continued increases in highly amplified jet stream flow, the conditions for lows to deepen rapidly and become very strong, will increase. Thus, we would expect greater frequencies of these downsloping wind events in Anchorage, overall, and strong winds from frontal passages to increase. Another hazard is strong cold, northerly winds from the interior, to a low in the Gulf of Alaska. Our subjective feeling is that these probably will weaken in intensity, somewhat. Driven by the fact that winter, bitter cold Arctic airmasses over the Interior won't be as deep and of long duration as they are currently.
Snow Storms and Freezing Rain:
Due to Anchorage's unique geography, cold air in winter continually, except only under the strongest of south flows, drains south through the Susitna Valley, from the Interior, after filtering through the gaps in the Alaska Range. This, combined to the proximity of the relatively warm waters of partially ice-covered Cook Inlet, occasionally allows heavy snowfall events to occur, when small lows form right over the Inlet, and move over the Bowl. In which 20-40 cm (8-16 inches) can fall in 24-48 hours. We expect these fairly infrequent events to remain so, since the colder air draining from the interior, will be warmer, as well.

Freezing rain events are another story entirely, however. We expect these to significantly increase over the coming decades to become a real problem, not just in Anchorage, but in most of mainland Alaska. Because in winter we are getting our strongest "meridional" flow patterns (strong southerly flow ahead of an upper-level ridge), which move very mild air north from the subtropics. This is how more heat is delivered to these higher latitudes, and thus, if the climate overall is going to continue warming, the pattern that is most responsible for this, will increase. A perfect example of this was the record-breaking ice storm of this past 21-23 November. Which paralysed Fairbanks with 20 mm (.80") of freezing rain, and Anchorage with about 14 mm. Coating all the roads with ice, causing numerous accidents and downed power lines. And unfortunately for Fairbanks, once that ice accumulated on the roads, it stayed there all winter! This freezing rain event, at one point, for three hours, was depositing ice accumulations from Seward, north, all the way to Barrow! Unprecedented in Alaska history.
http://akprogressive.blogspot.com/2010/11/dont-need-weatherman-and-matties-fourth.html







Wildfire:



The Anchorage Bowl specifically, doesn't experience nearly as many days of higher fire danger, than the interior, north of the Alaska Range, in spring or summer, due to the proximity of the waters of Cook Inlet, and Gulf of Alaska. Any kind of light to average flow from the southeast through southwest is moistened from these, and relative humidities during the day, are usually too high to dry the boreal forest out.

But occasionally, warm/dry spells in May to July can temporarily disrupt this pattern. When high pressure ridging builds directly over the region, and suppresses the local sea-breezes, and drier air from the north through east is forced in. We would expect an increase in this pattern, with stronger high pressure ridging, overall, but only a moderate increase. The other hazardous pattern that can produce higher fire danger, is when strong winds blow along the Chugach Front hill slopes, if the temperatures are high enough, and relative humidities, low enough. This occurs in the warm season, but infrequently. We would expect a moderate increase in these in the shoulder seasons, spring and fall, and slight increases in June and July. Due to the stronger low pressure sytems that would occur in Spring or Fall, having warmer airmasses than currently, and hence, lower relative humdities, in down-sloping winds. The Anchorage hillsides have very thick, tangled boreal forest vegetation, with extensive stands of dead and dying bug-killed white and black spruce trees, which could prove flashy and hazardous, in a very strong, and dry, downsloping wind event.
Thunderstorms:

The Anchorage Bowl usually only sees one or two weak thunderstorms, with just limited lightning, some small hail, and brief heavy rain, each late spring/summer. Some years none occur. This is because of the cool, stable air usually present at lower levels, chilled by the waters of the Gulf of Alaska and Cook Inlet, stabilises the lower atmosphere. Nonetheless, thunderstorm activity across Alaska as a whole has been increasing over the past 25 years, especially over the interior and Alaska Range. This is because, with the summer warming, and a resultant deeper troposphere (the lowest layer of the atmosphere in which all sensible weather occurs, usually 5-10 miles, or 8-16 KM deep, lower in winter), the lowest levels of the atmosphere become more unstable, and then, showers have the ability to become deeper, reaching higher heights, and hence stronger. Capable of generating lightning, as up and downdrafts in the deeper clouds are stronger. People on the Kenai Peninsula, and climbing rangers at Denali base camp, in the Alaska Range, have reported to your lead editor that they are now seeing thunderstorms each summer, when even 10-15 years ago, none ever occurred. I found this out the hard way when I did a 27 mile fast-pack on the Kesugi Ridge trail, in the Alaska Range, and was hit by lightning, when storms with continuous cloud-to-ground strikes overtook me. http://akprogressive.blogspot.com/2009/05/kesugi-ridge-experience.html. What we expect for Anchorage specifically then, are more episodes of stronger thunderstorms forming over the Chugach mountains, then drifting off and weakening over the Bowl, as they encounter cooler, stable lower-level maritime air. This happens in other coastal areas south down the North American continent.

This has been a quick, summary, of what we expect to see by 2051, here in Anchorage. This seems quite likely, as there is no coordinated, global effort to limit CO2 emissions, and unless the general socio-political systems in the "developed countries" change, there won't be for many decades. And the warming by 2090 will easily be doubled, from that in 2051. Cheers.