18 July 2017
I think I've pretty well figured it out. Speaking in terms of the Phanerozoic Era and a bit longer (750 million years or so), our planet is usually more than 7° Celsius warmer than today. The earth has already warmed almost 3° C, half of it before the industrial revolution.
We're still in an ice age now (the ice is just disappearing rapidly). The last ice age ended roughly 280 million years ago (they don't happen often). Humans have speeded up warming dramatically. The oceans are already up 300 feet from their ice age lows. They have 225 more feet to go.
Humans and our evolutionary progenitors have existed only during the ice age of the past 6-8 million years. We can probably extend the current cool period by not putting carbon into the atmosphere (though possibly not indefinitely, and at some point, it may be too late --- possibly now).
Climate is twice as variable when the planet is cooler (as it is now). When the planet is hot, it's basically hot everywhere, and probably too hot for human survival at the equator. The sun is gradually growing warmer. Thus the long-term trend over hundreds of millions of years is almost certainly going to be towards somewhat hotter temperatures.
Modern humans have walked the earth for only 200,000 years, 2/3 of that time only in Africa. It is possible, perhaps probable, that without the recent ice age, we couldn't have come to exist. We were almost extinguished as a species only 70,000 years ago. Could it happen again? We should be alert to the possibility.
Thinking over the next few centuries, I'm pretty sure we'll stop adding carbon to the atmosphere, and we'll probably start removing it. Fossil carbon is limited in supply, and we've already burned most of the easy-to-find fossil carbon. It would be better to use carbon to synthesize organic molecules. To our descendants, burning carbon for fuel will appear incomprehensible. Will the end of carbon burning stop global warming, at least for a while? Not in itself. However, I'm optimistic. I think the current (natural) warming trend can be reversed or slowed, though possibly only temporarily.
It's conceivable, perhaps likely, that humans may eventually learn how to manage global mean temperature for the benefit of biological diversity. The best way to start will be by developing non-carbon forms of energy generation. While solar and wind and other sustainable methods will be helpful, fusion power will eventually transform the power grid.
Though fusion power doesn't generate carbon as a waste product, it releases considerable levels of heat, and thus will still contribute to global warming. It will be better to get started on living without carbon sooner rather than later, but we will eventually need to learn how to manage all forms of human energy generation and to regulate global climate.
If the ice age norm of the past 6 to 8 million years can be sustained, our planet will remain more diverse. It may be that we can achieve this as a long-term climate goal. Much more examination of that question will need to take place than has so far occurred.
A positive and desirable multi-species outcome to the current problem of global warming is possible. We must remember that what we don't know is still markedly greater than what we do know. We have much to learn, and many important decisions to make.
_
We live in a complex, interactive, and increasingly borderless world in which our lives are impacted more than ever before by events occurring outside the sphere of our personal influence. I wish to establish a forum for the examination of these trends by presenting ideas which are central to the problem, disruptive of conventional thought, or conducive to leisure and conviviality.
Tuesday, July 18, 2017
Saturday, July 15, 2017
WHAT WAS THE EARTH'S CLIMATE LIKE WHEN THE GLOBAL MEAN TEMPERATURE WAS LAST AT 22° CELSIUS?
15 July 2017
I've been doing a little bit of research, based on the observation that humans are ice age creatures, even though ice ages have made up only 5% or so of our current era (roughly the past half billion years or so). So today's topic is, "What was the earth like during the much warmer climatic periods during which humans and our precursors hadn't yet evolved?" An implication of this discussion is that, due to human-initiated massive carbon release, we might be headed back to such conditions sooner rather than later (that is, in a few hundred years, vs. several million years).
I've been doing a little bit of research, based on the observation that humans are ice age creatures, even though ice ages have made up only 5% or so of our current era (roughly the past half billion years or so). So today's topic is, "What was the earth like during the much warmer climatic periods during which humans and our precursors hadn't yet evolved?" An implication of this discussion is that, due to human-initiated massive carbon release, we might be headed back to such conditions sooner rather than later (that is, in a few hundred years, vs. several million years).
The underlying question we're
asking is, "Did the earth have to cool before humans could emerge?"
Our working hypothesis is that humans are specialists in handling ecological
and climatic diversity, and that the "hot" earth that is more typical
of the last several hundred million years lacked the diversity that may have
been needed for humans and our precursors to evolve. It is notable that even
our evolutionary forebears don't show up in the fossil record until the earth
transitioned into its most recent ice age (we're technically still in it) about
6 million years ago. Homo Sapiens has about a 200,000 year history, and our
genus (homo) has been around for only about 2-1/2 million years.
Well, let's take as an example the
late Cretaceous period, roughly 65 to 100 million years ago, and just preceding
the extinction of the dinosaurs: In general, the climate of the Cretaceous
Period was much warmer than at present, perhaps the warmest on a worldwide
basis than at any other time during the past 542 million years (the Phanerozoic
Eon). No ice existed at the poles. The oceans were stagnant and similar to hot
springs in temperature. Dinosaurs migrated between the Warm/Hot Temperate and
Cooler (extreme north and south) Temperate Zones as the seasons changed. High
temperature conditions were almost constant until the end of the period. The
warming may have been due to intense volcanic activity which produced large
quantities of carbon dioxide.
Floral evidence suggests that
tropical to subtropical conditions existed as far as 45° N, and temperate
conditions extended to the poles.
Large magma deposits were
sufficient to raise sea levels to extremely high elevations, creating vast,
shallow seas across the continents. The Tethys Sea connecting the tropical
oceans east to west also helped to warm the global climate. Warm-adapted plant
fossils are known from localities as far north as Alaska and Greenland, while
dinosaur fossils have been found within 15 degrees of the Cretaceous south
pole.
An equable temperature gradient
from the equator to the poles (one-half that of the present) meant much less
climatic variability than today, and weaker global winds, which drive the ocean
currents, resulted in less upwelling and more stagnant oceans than today. This
is evidenced by widespread black shale deposition and frequent anoxic events.
Sediment cores show that tropical sea surface temperatures may have briefly
been as warm as 42° C (108° F), 17° C (31° F) warmer than at present, and that
they averaged around 37° C (99° F). Meanwhile, deep ocean temperatures were as
much as 15 to 20° C (27 to 36° F) warmer than today's.
As to geography, the continents had
differentiated from Pangaea, but were bunched together more closely than today.
A vast watery channel divided North America north to south, with only the Rocky
Mountains above the sea in the west. Despite sea levels more than 200 feet
higher than today, Antarctica and Australia were still one continent. India was
an island located east of Madagascar. There was much more sea surface, and much
less land surface.
So, there are two questions to wrap
up: (1) Is there any particular reason that our human precursors waited until the climate described above had cooled by about 10° C before showing up? (2) Are humans
and other species going to adapt well to a planet that is 7-8° C warmer than
today?
The scientist I have so far identified who seems most interested in this question is Dr. Rick Potts at the Smithsonian Institution. The following is an abstract for one of his journal articles.
THE RICK POTTS HYPOTHESIS
Variability selection (abbreviated as VS) is a process considered to link adaptive change to large degrees of environment variability. Its application to hominid evolution is based, in part, on the pronounced rise in environmental remodeling that took place over the past several million years. The VS hypothesis differs from prior views of hominid evolution, which stress the consistent selective effects associated with specific habitats or directional trends (e.g., woodland, savanna expansion, cooling). According to the VS hypothesis, wide fluctuations over time created a growing disparity in adaptive conditions. Inconsistency in selection eventually caused habitat-specific adaptations to be replaced by structures and behaviors responsive to complex environmental change. Key hominid adaptations, in fact, emerged during times of heightened variability. Early bipedality, encephalized brains, and complex human sociality appear to signify a sequence of VS adaptations—i.e., a ratcheting up of versatility and responsiveness to novel environments experienced over the past 6 million years. The adaptive results of VS cannot be extrapolated from selection within a single environmental shift or relatively stable habitat. If some complex traits indeed require disparities in adaptive setting (and relative fitness) in order to evolve, the VS idea counters the prevailing view that adaptive change necessitates long-term, directional consistency in selection. © 1998 Wiley-Liss, Inc.
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The scientist I have so far identified who seems most interested in this question is Dr. Rick Potts at the Smithsonian Institution. The following is an abstract for one of his journal articles.
THE RICK POTTS HYPOTHESIS
Variability selection (abbreviated as VS) is a process considered to link adaptive change to large degrees of environment variability. Its application to hominid evolution is based, in part, on the pronounced rise in environmental remodeling that took place over the past several million years. The VS hypothesis differs from prior views of hominid evolution, which stress the consistent selective effects associated with specific habitats or directional trends (e.g., woodland, savanna expansion, cooling). According to the VS hypothesis, wide fluctuations over time created a growing disparity in adaptive conditions. Inconsistency in selection eventually caused habitat-specific adaptations to be replaced by structures and behaviors responsive to complex environmental change. Key hominid adaptations, in fact, emerged during times of heightened variability. Early bipedality, encephalized brains, and complex human sociality appear to signify a sequence of VS adaptations—i.e., a ratcheting up of versatility and responsiveness to novel environments experienced over the past 6 million years. The adaptive results of VS cannot be extrapolated from selection within a single environmental shift or relatively stable habitat. If some complex traits indeed require disparities in adaptive setting (and relative fitness) in order to evolve, the VS idea counters the prevailing view that adaptive change necessitates long-term, directional consistency in selection. © 1998 Wiley-Liss, Inc.
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Labels:
difficult issues,
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secular trends
HUMANS AS AN ICE AGE SPECIES II
15 July 2017
Scientists have recorded five significant ice ages
throughout the Earth’s history: the Huronian (2.4-2.1 billion years ago),
Cryogenian (850-635 million years ago), Andean-Saharan (460-430 mya), Karoo
(360-260 mya) and Quaternary (2.6 mya-present). Approximately a dozen major
glaciations have occurred over the past 1 million years, the largest of which
peaked 650,000 years ago and lasted for 50,000 years. The most recent
glaciation period, often known simply as the “Ice Age,” reached peak conditions
some 18,000 years ago before giving way to the interglacial Holocene epoch
11,700 years ago.
That humans arose during an ice age
may be due to chance, but over the last 750 million years, the chances of a
species emerging in an ice age (global mean temperature ~12C) would have been
roughly 5%, as the planet is hot (~22C) something like 80% of the time.
(Mammals showed up 220m years ago in the late Triassic, one of many warm/hot
periods.)
Obviously species have had
successes against longer odds than that. However, my working hypothesis is that
there is more ecological diversity during ice ages (though not snowball earth
of 650m years ago). If the earth usually has palm trees and crocodiles in the
arctic circle, then there would be a lot less maple, walnut and apple trees
elsewhere. This is not to say that humans did not originate in the tropics, as
it seems we did, and there is a lot about the transition from forest to savanna
that I don't know much about. Also, the African drought-induced near-extinction
was apparently overcome by moving to the seashore, which gets you into the
aquatic ape and ecosystem boundary hypotheses.
Keep in mind that the planet was
2-3 C colder then than it is now, and a bit more than half the difference is
pre-industrial (most sea level rise has been/will be preindustrial). I think
it's clear on the 750m year chart that we have been in a warming phase since we
became tool and technology users, at the very least. So global warming was
already happening, though I think it's obvious that this is the first time in
geological history that fossil carbon has been burned. Thus, this cycle can go
(and obviously is going) faster and possibly higher than in the past. Other
causes of climatic variation include fluctuations in solar intensity,
atmospheric clarity and orbital variations (Milankovitch), but the big cycle
seems to be carbon-driven, which in my view is the strongest single argument
that humans putting carbon into the atmosphere is changing things (that is,
accelerating an existing trend). In fact, it is bluntly an irrefutable argument
if you study geological history.
One can also see that at least 8
degrees C of the big fluctuations happen very quickly (less than 1 million
years) in geological terms. I honestly believe (1) that if we don't get
smarter, we'll move from 15 to 22C in only a few hundred years (a new
geological record), as that will put all the carbon there is into the atmosphere,
but also (2) given a few hundred years, we will get much smarter and actually
more or less totally eliminate carbon burning, or at least highly restrict it,
and that much sooner than that, we'll have the technologies to capture carbon
and take it back out of the atmosphere (no UN bureaucracy or carbon credit
system needed, because we'll be rich enough that we can easily afford it).
Note that around 13-14C is where
the bigger/faster moves usually happen anyway, as that is enough to get the
positive feedbacks going with methane, forest fires, tectonic rebalancing, etc.
That is, whatever the bureaucrats may think, we've been past the breakaway
threshhold for some time already.
So let's just say that humans had
tried to get their start at 22C, which would take you roughly to 35m years ago.
There would have been no coral reefs, the entire equatorial region would have
been uninhabitable (>120F), and there would have been only tropical and
desert ecosystems. I'm pretty sure it would have been a less diverse world,
which is not to say that tropical systems are not diverse.
It is probably also not
accidental that we are post Cretaceous-Paleogene extinction creatures (66ma),
as the meteor impact that extinguished 75% of earth's life forms occurred at
the height of the last warm period, which also (perhaps meaningfully) marked
the rise of mammals, though it was still very hot for another 40m+ years after
the mass extinction (there is also a current mass extinction being driven by
human modification of all planetary ecosystems). The meteor impact at 66ma
doesn't even show up on the longterm climatic cycle chart, but it would have
been very cold for a very short time, geologically.
Importantly, humans didn't show
up, even our precursors (who emerged no more than 6m years ago), until
temperatures dipped down to ice age levels. However, Haplorrhini (apes,
monkeys, tarsiers) are a human precursor who showed up immediately post
extinction event (63ma), so maybe that is also meaningful.
Finally, the real advances in
human technology have occurred in only the last few thousand years, which has
been a period of significant glacial retreat (warming with positive feedbacks
engaged long before industry started). I have just refreshed myself on Lake
Agassiz, which oversat Kenora, Ontario (where I live) as well as most of central Canada and the North
Central US. Interestingly, the central North American glaciers melted for
thousands of years without sea level rise, because the lake was held back by a
glacial dam that first broke about 13,000 years ago, then reformed, and had its
last break about 8000 years ago (both events raised sea levels several feet,
and one or both may account for the multicultural flood narratives).
The rupturing of Lake Agassiz is
linked to the rise of systematized agricultural in Europe which enabled the rise
of cities, and that is also dependent on the Atlantic Meridional Overturning
Circulation (AMOC), which sustains moderate European temperatures, but which
has reduced 30% since 1957, associated with increased warming-induced
freshwater flows into the Arctic Ocean, and thus with southward flows into the
Atlantic (conversely, the Arctic Ocean is shrinking due to warm water
penetration further north). On a positive note, when the AMOC reduces, we have
fewer Atlantic hurricanes. On the downside, Europe would turn much colder very
quickly if the circulation turns southwards (it currently forks, and half flows
north around Europe, and half flows towards West Africa.
As to unanswered questions, human
have obviously benefited by the plummeting of global temperatures to their
lowest historic levels perhaps 6-8 million years ago, but we have also
capitalized on the bounceback to warmer temperatures, which coincides with
hominid evolution over the last 2-1/2 million years. In brief, it appears that
humans thrive when ecosystems are multiple and diverse, and my best guess is
that the Quaternary Ice Age created the exact types of increasing diversity on
which emerging humans eventually capitalized.
_
Labels:
difficult issues,
science,
secular trends
Thursday, July 13, 2017
IS THERE A REASON WHY HUMAN EVOLUTION OCCURRED DURING A RARE GLOBAL ICE AGE?
13 July 2017
I have become intrigued with the fact that modern humans
emerged roughly 2.5 million years ago, at the absolute temperature bottom of
one of the earth's relatively rare cold climatic periods (making up only 5% of the last 3/4 billion years or so). That is, we are
unarguably ice-age creatures. I've found a couple of new charts that illustrate
the link between human emergence and cold climate. Interestingly, a Google
search on the subject doesn't really turn up anything beyond this.
If you look at the link between
human evolution and climate, you get articles explaining how climatic variability may have prompted aspects of human evolution --- tool-making,
language, an enlarged brain case, etc., but we're talking in these cases about
variabilities in maybe a degree or two of global mean temperature, which is
small stuff if you look at the longer-term climatic record of our planet, where
there is evidence of 12-25° Celsius variation in global mean temperature
(today's mean temperature is in the 14-15° C range --- still near its 12° C low
of 2-5 million years ago.
I also tried a search about humans
as ice-age creatures, and literally all that comes up are endless articles
about how hungry humans caused the extinction of the large ice-age mammals.
An examination of global mean
temperatures over the past 700 million years makes clear that only about 35
million of those years were typified by today's still very low global mean
temperature in the range of 12-15° C (recently warming dramatically, as
everyone knows).
Note that the earth's mean
temperature is much more often in the 22° C range --- with 450-500 million of
the past 700 million years at or near that level. Strikingly, the transitions
occur rapidly in geological time, with upward or downward spikes of maybe 8° C
occurring in the space of roughly a million years (maybe less?). Positive
feedback loops --- as we are seeing today --- very likely account for those
geologically rapid transitions.
How will humans fare when, in less
than another millions years --- and possibly in only a few centuries, the
planet goes back to its 22° C climatic norm (or possibly higher)? The process is gradual in individual human
years, but currently extremely rapid in geological and generational terms. Our children's children will
certainly be living with the ever more dramatic consequences of the current
human-induced "carbon era."
As an optimist, I believe we can
resolve most or all of the problems associated with a rapid return to a much
hotter planet. However, we'll have to be considerably more focused than at
present to accomplish the necessary ameliorations and accommodations.
Based on my reading to date, we'll do best to hold back the natural and at some point inevitable return to much warmer global mean temperatures. This will enable us to save the coral reefs as well as many other species, to preserve maximum species diversity, to keep our coastal and tropical cities where they are, and to contain northward-migrating tropical and temperate region diseases. To accomplish this, we will require fusion as well as solar power, and we'll have to put robots to work to aid us in maintaining and repairing the environments and systems we have damaged.
This article provides the best summary of earth's long-term climatic variation that I have found: click here.
_
Labels:
difficult issues,
science,
secular trends
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