Over the past weeks, we have witnessed extreme weather events occurring in the present, examined how extreme event trends may alter in the future, and how they have appeared to change from past to present. When it comes to predicting the future, however, I hope I emphasised how uncertain these projections and speculations are: I found this article on the BBC News just today questioning current climate model data..
http://www.bbc.co.uk/news/science-environment-20947224
Saying this, there is the general consensus within the scientific community that events such as hurricanes and coastal flooding are to increase in some regions in the future. Predictions can only be as good as current model data, and at the moment it is agreed we are living in a warming world. This will lead to rising sea levels, higher levels of moisture uptake into the atmosphere and warmer oceans.
Unfortunately, all of these factors add to an increased chance of hurricane formation and flooding...so keep hold of your hats!!
Keep hold of your hats!
Wednesday, 9 January 2013
Tuesday, 8 January 2013
And now a look back in time...
Looking at past global climate helps scientists to gain an
overall picture of climate variability; studying past events aids in
discovering whether present day climate is becoming more unpredictable, or
whether it is part of a longer trend. This study carried out by Zheng et al. (2006) aims to reconstruct the climate of eastern China over the past 1500 years using
a combination of different proxies. In order to do this, a new dataset was
constructed out of 3 sets of historical data: this is not ideal as different sourcing
techniques were used and so the dataset could contain error or inconsistences
(it is noted that there are many missing records before 1470).
In order to overcome this problem, Zheng et al. produced a
Dry-Wet Index which analyses the long term change in precipitation instead of
analysing individual records. This would help to decrease the error within the
dataset and to focus on climate variability trends. The study area was divided
into 3 regions based on their climatic differences, so that the natural
occurrence of precipitation did not impact too much on the study; the aim was
to find the variation in precipitation so it had to be accounted for that some
regions were naturally wetter than others.
Of course, it was found that the dry-wet cycle within
eastern China varied considerably over the past 1500 years (please refer to the
article). But what about what we’re really interested in here, extreme weather?
The results from the study indicated that 18 flood events
occurred within eastern China between 501-2000, with a 4 year flooding event
occurring 1422-1425. Three major wet epochs were identified 880s-990s,
1240s-1420s and 1540s-1910s. Of course, there was variation in the climate
within these times too. The occurrence of flooding has continued into the last
300 years, although the number of extreme droughts has decreased. Perhaps this
is a sign of the changing climate? It has been said that the monsoon cycle is
intensifying, could it perhaps be possible that these records are reflecting
this?
By looking at the figure above, taken from Zheng et al., it
can clearly be seen that the frequency and severity of droughts (indicated by
the red bar) is decreasing as the records near the present day. The flood
occurrences (blue), however, appear to becoming more frequent and are just as
severe (indicated by the bar width) as those occurring in the past 1500 years.
Although there has to be some allowances made for the dataset used, with better
records obviously available towards modern day, the general trend does infer
that eastern China is generally becoming more vulnerable to extreme flood
events.
In my opinion, these results concur with recent research
that the hydrological cycle is intensifying in light of global warming (Duracket al. (2012)). This will likely increase the intensity
of the monsoon (Ruosteenoja 2003) as with a warmer atmosphere which has a
greater ability to absorb moisture, and higher evaporation rates occurring from
warmer ocean surface waters (Cubasch et al. 2001) there is greater potential
for precipitation. Currently the monsoonal rains occur from June to September,
but in a warmer world this window could widen. Add to this the fact that sea
levels are rising due to increased melt water and thermal expansion (Cubasch et
al. 2001) and it is easy to see how the likelihood of extreme flood events
seems to be increasing. Of course, it is extremely difficult to predict how our
climate will alter in the future, but at the moment, the trends are all heading
in the same direction…
Sunday, 6 January 2013
The future of the hydrological cycle
'A change to freshwater availability in response to climate change poses a more important risk to human societies and ecosystems than warming alone. Changes to the global water cycle and the corresponding redistribution of rainfall will affect food availability, stability, access, and utilization.'
You may think that looking at the hydrological cycle in the future is going a little off topic when it comes to extreme weather events; but a rise in ocean temperatures could offer a greater possibility of hurricane formation over surface waters, and a rise in sea level creates a higher level of vulnerability for coastal populations. It is all connected.
I've linked a recent article by Durack et al. to this post, which caused quite a stir when it was published in Science (2012), as it proposed that for every 1°C warming in surface temperature, the hydrological cycle could intensify by 8(+/-5)%. This means that a 2°C warming in the future, (which isn't unlikely at the current rate of GHG consumption) could see a 24% intensification of the hydrological cycle. This would affect the entire globe, with current wet regions receiving more precipitation and those regions that are drier experiencing more frequent drought.These results were generated by Durack et al. by running sea surface salinity (SSS) data with current climate estimates (CMIP3 scenarios). In my opinion, SSS is a sensible measure to use as it correlates highly with evaporation-precipitation patterns and is far more reliable than the precipitation records; which offer scarce coverage over the oceans and may contain error in gathering techniques (e.g. satellite readings). The higher the salt content observed, the higher evaporation rates.
Of course studies such as this one have been conducted in the past, but the recent CMIP3 scenario data that this model ran with offers a more accurate view of global climate dynamics than has been used previously. Other models ran with more simplistic datasets: as we all know the climate system is very complicated, so leaving out one small factor can impact heavily on results. Of course, the CMIP3 scenarios aren't perfect, but they are the best we have.
The purpose of me drawing your attention to this article is the fact that it is possible that the 1°C of warming that we have experienced over the last century is having a greater impact than we imagine. Although the findings of this study are quite controversial, and in some cases are the complete opposite of other studies; I think that this experiment has ground to stand on. The reasoning behind using SSS as a representative factor of E-P is sensible and the scenario this data was run with is the best that is available. Durack infers that during the last 50 years, the water cycle has amplified by 4%: with another 1°C warming, it could be amplified by a further 8%. This would greatly increase the likelihood of flooding and hurricane formation.
So, as I said, this may have been a little off topic, but I hope you can see how it is an important in relation to the subject. I think Durack et al.'s paper is insightful and although it is definitely not the only work on the subject out there, I hope you can see how it makes a strong case. Anyhow, it's a nice read and also makes you think about how our actions are influencing tomorrow's world, so enjoy...
Thursday, 3 January 2013
Its raining again
Welcome back, hope you enjoyed the festive season. As the video on the previous post highlighted, there has been a recent increase in flooding (amongst other extreme events) in the UK. After having studied Robson's article 'Evidence for trends in UK flooding' I will decide whether or not it is likely that these events have been caused by climate change.
A scene from a small village in York after the flooding in February 2010- could the UK see more of this as the climate changes?
A scene from a small village in York after the flooding in February 2010- could the UK see more of this as the climate changes?
Robson’s 2002 study of trends in UK flooding emphasises how
difficult it is to distinguish whether or not climate change is impacting on
our weather conditions. Although some trends have indeed shown that winter
rainfall and number of high flow days is increasing, this can not necessarily
be attributed to climate change. Instead it can be attributed to natural
climate variability, which can see short term changes in local weather
conditions; but when trends are averaged over time, the average climate
conditions have remained in a stable state. Unfortunately, although Robson did
find evidence of increasing rainfall rates, the data series in the UK is not
long enough (~60 years of appropriate coverage), nor reliable enough to rule
out the cause being climate variability. Other factors such as changing land use can affect flooding records, especially when the changes involve
urbanisation or agriculture as these can impact greatly on infiltration rates. This is why an urban environment is at greater risk of flooding.
So, although Robson did find evidence of increasing rainfall
and number of high flow days in the UK, with the results from Scotland closely
echoing the trends found in previous studies; climate change cannot be assigned
as the cause, as other factors can’t be ruled out. In my opinion, however, with
similar events happening around the globe; it is more likely that the main driver is the climate, whether it is just varying in the short term,
or changing in the long term. For me, it is preferable to note this as the cause rather than change in landuse, although it is noted that this does play a role. Either way, due to this, the UK is experiencing
more extreme weather events today than it has done in the past.
Wednesday, 19 December 2012
If you've got a spare hour or so...
So during the research for my next post I found this video which I thought some could find quite interesting. It's basically an overview of the climatic extremes that Britain has experienced within the past decade or so, and in my opinion it justifies the concerns that weather patterns are becoming more unpredictable. So have a look if you have time and judge for yourself...
http://www.youtube.com/watch?v=SbTc6LZ9KZ4
http://www.youtube.com/watch?v=SbTc6LZ9KZ4
Monday, 3 December 2012
A look into the future
I am well aware that over the course of these past few weeks
I have been talking on the topic of anthropogenic climate change; and as yet, I
still haven’t fully explained either what this is seen to be, or the future it
could potentially lead to. To give a brief overview, here is a video looking at
some effects of climate change, focussing on 3 of the IPCC SRES scenarios.
Please be aware that these scenarios were predicted 12 years ago and that a renewed report is to be released in the next 6 months or
so.
There are high levels of uncertainty in future climate predictions,
due to the complexity of the environment being hard to replicate in models and
also a lack of knowledge in how the globe is going to respond to future
changes. Therefore, climate change is still a contentious issue within the
scientific community. There are some general trends that have been agreed upon,
however, which include the fact that our globe is going to get warmer (1.4-5.8°C by the end of the 21st
century).
As can be presumed, an increase in temperature would see a
similar increase in the frequency of heatwave events, such as that seen in
Europe in 2003- this could be seen as a cool summer by 2100! A change in
temperature could also lead to changes in the water content of the atmosphere,
as saturation vapour pressure increases with heat. This could lead to more
frequent, heavy precipitation events in some places which leave some regions vulnerable to flooding, especially coastal populations (e.g in Bangladesh).
The Thermohaline Circulation will almost certainly be affected in our future world, as increased precipitation events in some regions (e.g Europe) could lead to an increased uptake of freshwater within the circulation; decreasing the density of surface waters and therefore the likelihood that this water will sink, weakening the THC. This could also be exacerbated by the melting of the Greenland ice sheet, where the large influx of freshwater would severely slow the circulation down or even halt it, leading to changes in heat transport around the globe.
All of these changes will impact different regions in different ways, but are likely to increase the likelihood of tropical storms, heatwaves, droughts and flooding depending on the country.
As I mentioned before, the future climate is still very unclear although scientists are always gaining further insight. The IPCC SRES scenarios are widely used as a basis for climate modelling and are perhaps the most reliable projections that we currently have, however, these have been updated recently and are to be released in a future report. As such, it is difficult to judge whether or not these documents can provide us with accurate facts about global climate in the future, but for the present, assumptions as to how global feedbacks will react to forcings is the best we can hope for. After examining these articles, however, I think it is safe to say that our globe will warm and that this will affect the frequency of extreme events. The extremities of the changes are yet to be seen...
Friday, 23 November 2012
Here's a little article...
It appears that I'm not the only one thinking of the possible impacts that our actions will have on future climate. The BBC reported on the effects of climate change already being evident in Europe, ahead of the UN Climate Convention in Qatar starting on Monday.
In agreement that the frequency and intensity of extreme weather events are going to increase (with some of the areas to be hit hardest also those less than able to cope) the report acknowledges that the cost of damages caused by extreme events is already increasing, in part due to larger populations and more infrastructure in vulnerable areas. But it begs the question, how are we going to cope in our future world? The UN convention hopes to address the current and future state of our climate as well as assessing possible adaptation and mitigation techniques. Have we passed the point where we can curb our carbon emissions, meaning that mitigation and adaptation are our sole defences?
Have a think, read the article, and I'll follow this with another post shortly.
http://www.bbc.co.uk/news/science-environment-20408350
In agreement that the frequency and intensity of extreme weather events are going to increase (with some of the areas to be hit hardest also those less than able to cope) the report acknowledges that the cost of damages caused by extreme events is already increasing, in part due to larger populations and more infrastructure in vulnerable areas. But it begs the question, how are we going to cope in our future world? The UN convention hopes to address the current and future state of our climate as well as assessing possible adaptation and mitigation techniques. Have we passed the point where we can curb our carbon emissions, meaning that mitigation and adaptation are our sole defences?
Have a think, read the article, and I'll follow this with another post shortly.
http://www.bbc.co.uk/news/science-environment-20408350
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