Saturday, April 26, 2014

M5.1 Earthquake hits Greenland Sea

An earthquake with a magnitude of 5.1 on the Richter scale hit the Greenland Sea on April 26, 2014, at 03:55:33 UTC at a depth of 10.00 km (6.21 mi). The epicenter of the earthquake is located right on the faultline that crosses the Arctic Ocean, at 73.479°N 7.974°E, some 567km (352mi) SSW of Longyearbyen, Svalbard.

[ click on image to enlarge ]
This follows four further recent earthquakes close to Svalbard or on the faultline north of Greenland, as indicated on above map. All these earthquakes struck at a depth of 10.00 km (6.21 mi).

Some of these earthquakes have also been discussed in earlier posts:
M4.6 - North of Franz Josef Land, 2014-04-13 02:12:19 UTC, also discussed in this post
M4.2 - North of Franz Josef Land, 2014-04-04 07:01:30 UTC
M4.4 - 262km NE of Nord, Greenland, 2014-04-22 10:30:23 UTC, also discussed in this post
M4.3 - 148km SSE of Longyearbyen, Svalbard, 2014-04-24 08:33:06 UTC
M5.1 - Greenland Sea, 2014-04-26 03:55:33 UTC
M4.5 - Gakkel Ridge, 2014-03-06 11:17.17.0 UTC, also discussed in this post

There have been a large number of earthquakes around Greenland since early 2014, as illustrated by the image below. This could be an indication of isostatic rebound, as also discussed in this earlier post.

[ click on image to enlarge ]

As melting of the Greenland Ice Sheet speeds up, isostatic rebound could cause earthquakes around Greenland to become stronger and occur more frequently. Earthquakes in this region are very worrying, as they can destabilize hydrates contained in the sediment under the seafloor of the Arctic Ocean. Furthermore, one earthquake can trigger further earthquakes, especially at locations closeby on the same faultline.




Related

- M4.4 Earthquake hits Arctic Ocean north of Greenland

- M4.5 Earthquake hits Arctic Ocean
http://arctic-news.blogspot.com/2014/04/m45-earthquake-hits-arctic-ocean.html

- Earthquakes in the Arctic Ocean
http://arctic-news.blogspot.com/2014/04/earthquakes-in-the-arctic-ocean.html

- Methane, Faults and Sea Ice
http://arctic-news.blogspot.com/2013/11/methane-faults-and-sea-ice.html

- Norwegian Sea hit by 4.6M Earthquake
http://arctic-news.blogspot.com/2013/11/norwegian-sea-hit-by-46m-earthquake.html

- Greenland Sea hit by M5.3 Earthquake
http://arctic-news.blogspot.com/2013/10/greenland-sea-hit-by-m53-earthquake.html

- Earthquake hits waters off Japan
http://arctic-news.blogspot.com/2013/10/earthquake-hits-waters-off-japan.html

- Earthquake hits Laptev Sea
http://arctic-news.blogspot.com/2013/09/earthquake-hits-laptev-sea.html

- Methane Release caused by Earthquakes
http://arctic-news.blogspot.com/2013/09/methane-release-caused-by-earthquakes.html

- Earthquake M6.7 hits Sea of Okhotsk
http://methane-hydrates.blogspot.com/2013/10/earthquake-m67-hits-sea-of-okhotsk.html

- Sea of Okhotsk
http://methane-hydrates.blogspot.com/2013/06/sea-of-okhotsk.html

- Seismic activity
http://arctic-news.blogspot.com/p/seismic-activity.html

- Climate Plan
http://climateplan.blogspot.com




Tuesday, April 22, 2014

M4.4 Earthquake hits Arctic Ocean north of Greenland

An earthquake with a magnitude of 4.4 on the Richter scale hit the Arctic Ocean north of Greenland on April 22, 2014, at 10:30:23 UTC at a depth of 10.00 km (6.2 mi).

[ click on image to enlarge ]
The epicenter of the quake is located right on the faultline that crosses the Arctic Ocean, at 83.328°N 4.568°W, 262km (163mi) NE of Nord, Greenland.

The earthquake follows another earthquake that hit the Arctic Ocean closeby on this faultline, on April 13, 2014, north of Franz Josef Land.

Earthquakes at this location are very worrying, as they can destabilize hydrates contained in the sediment under the seafloor of the Arctic Ocean. Furthermore, one earthquake can trigger further earthquakes, especially at locations closeby on the same faultline.




Related

- M4.5 Earthquake hits Arctic Ocean
http://arctic-news.blogspot.com/2014/04/m45-earthquake-hits-arctic-ocean.html

- Earthquakes in the Arctic Ocean
http://arctic-news.blogspot.com/2014/04/earthquakes-in-the-arctic-ocean.html

- Methane, Faults and Sea Ice
http://arctic-news.blogspot.com/2013/11/methane-faults-and-sea-ice.html

- Norwegian Sea hit by 4.6M Earthquake
http://arctic-news.blogspot.com/2013/11/norwegian-sea-hit-by-46m-earthquake.html

- Greenland Sea hit by M5.3 Earthquake
http://arctic-news.blogspot.com/2013/10/greenland-sea-hit-by-m53-earthquake.html

- Earthquake hits waters off Japan
http://arctic-news.blogspot.com/2013/10/earthquake-hits-waters-off-japan.html

- Earthquake hits Laptev Sea
http://arctic-news.blogspot.com/2013/09/earthquake-hits-laptev-sea.html

- Methane Release caused by Earthquakes
http://arctic-news.blogspot.com/2013/09/methane-release-caused-by-earthquakes.html

- Earthquake M6.7 hits Sea of Okhotsk
http://methane-hydrates.blogspot.com/2013/10/earthquake-m67-hits-sea-of-okhotsk.html

- Sea of Okhotsk
http://methane-hydrates.blogspot.com/2013/06/sea-of-okhotsk.html

- Seismic activity
http://arctic-news.blogspot.com/p/seismic-activity.html

- Climate Plan
http://climateplan.blogspot.com

Arctic Sea Ice in Steep Descent

Arctic sea ice area is in steep descent, as illustrated by the image below. Sea ice area was only smaller at this time of the year in 2007, for all years for which satellite data are available.

[ click on image to enlarge ]
Earlier this year, on March 9, 2014, Arctic sea ice area was at a record low for the time of the year. Since then, area did show some growth for a while, to the north of Scandinavia. This growth could be attributed largely to strong winds that made the sea ice spread with little or no growth in volume. The 30-day Naval Research Laboratory animation below shows recent sea ice speed and drift.


Indeed, sea ice volume in March 2014 was the 2nd lowest on record. Only March 2011 had a lower volume as discussed in a recent post. The 30-day Naval Research Laboratory animation below shows recent sea ice thickness. 



Low sea ice volume and area jointly suggest there could be a total collapse of the sea ice later this year, in line with observation-based non-linear trends. For years, this blog has warned that observation-based projections point at Arctic sea ice disappearance within years, with dire consequences for the Arctic and for the world at large.

As said, winds are responsible for much of sea ice variability, and winds could either slow down or speed up such a collapse. On this point, it's good to remember what Prof. Peter Wadhams said in 2012:
". . apart from melting, strong winds can also influence sea ice extent, as happened in 2007 when much ice was driven across the Arctic Ocean by southerly winds. The fact that this occurred can only lead us to conclude that this could happen again. Natural variability offers no reason to rule out such a collapse, since natural variability works both ways, it could bring about such a collapse either earlier or later than models indicate.

In fact, the thinner the sea ice gets, the more likely an early collapse is to occur. It is accepted science that global warming will increase the intensity of extreme weather events, so more heavy winds and more intense storms can be expected to increasingly break up the remaining ice, both mechanically and by enhancing ocean heat transfer to the under-ice surface."
The image on the right, produced with NOAA data, shows mean coastal sea surface temperatures of over 10°C (50°F) in some areas in the Arctic on August 22, 2007.

In shallow waters, heat can more easily reach the bottom of the sea. In 2007, strong polynya activity caused more summertime open water in the Laptev Sea, in turn causing more vertical mixing of the water column during storms in late 2007, found a 2011 study, and bottom water temperatures on the mid-shelf increased by more than 3°C (5.4°F) compared to the long-term mean.

Another study found that drastic sea ice shrinkage causes increase in storm activities and deepening of the wind-wave-mixing layer down to depth ~50 m (164 ft) that enhance methane release from the water column to the atmosphere. Indeed, the danger is that heat will warm up sediments under the sea, containing methane in hydrates and as free gas, causing large amounts of this methane to escape rather abruptly into the atmosphere.

Such warming would come on top of ever-warmer water that is carried by the Gulf Stream into the Arctic Ocean and that has already been blamed for large methane releases from the seafloor of the Arctic Ocean last year.

The prospect of an El Niño event, as discussed in an earlier post, makes the situation even more dire.

The consequences of sea ice collapse will be devastating, as all the heat that previously went into transforming ice into water will be asbsorbed by even darker water, from where less sunlight will be reflected back into space. The danger is that further warming of the Arctic Ocean will trigger massive methane releases that could lead to extinction at massive sclae, including extinction of humans.

Hopefully, more people will realize the urgency of the situation and support calls for comprehensive and effective action as discussed at the Climate Plan blog.



Links

- March 2014 Arctic Sea Ice Volume 2nd Lowest On Record
http://arctic-news.blogspot.com/2014/04/march-2014-arctic-sea-ice-volume-2nd-lowest-on-record.html

- Supplementary Evidence by Professor Peter Wadhams
http://arctic-news.blogspot.com/2012/04/supplementary-evidence-by-prof-peter.html

- Has the Descent begun?
http://arctic-news.blogspot.com/2014/03/has-the-descent-begun.html

- Nea-term Human Extinction
http://arctic-news.blogspot.com/2014/04/near-term-human-extinction.html

- Climate Plan blog
http://climateplan.blogspot.com


Friday, April 18, 2014

Data analysis: ten tips I wish I'd known sooner





I enjoy analysing data and I've been doing it for years, but I still do things inefficiently. All the same, I have learned some things along the way. As I work through another complex dataset, I thought it worth sharing some of the most useful tips I've picked up to make life simpler and smoother.  Some are very elementary and they will mostly be of relevance to psychologists who use Excel and SPSS to do fairly straightforward analyses, though some points are more generic.



A lot of these tips have to do with deploying those frontal lobes and thinking ahead: you need to be aware of three things:


  • How you set up a dataset can make a big difference to how easy it is to analyse later on

  • You will not remember anything about your data in a few years (or even months) time

  • There are increasing moves towards data-sharing - i.e. making your data available on a public repository and you need to plan for that too.



1. Label your subjects consistently and anonymously


You will almost certainly be required to anonymise data collected from human subjects. It is amazing how often people sign up to this in their ethics application but then forget all about it. I've seen supposedly anonymised data identified by people's names, initials and/or dates of birth. Don't do it!



I find simple consecutive number codes work fine, with a prefix denoting which study the subjects  come from. There are two things to think about, in addition to anonymisation. First, will it be useful to be able to sort subjects by code number into specific groups? For instance, if you have three groups identified as young, middle-aged and old, you might think of labelling them with Y1, Y2, .... M1, M2 etc.  But in certain computing systems, this will mean that when you generate output, e.g. means for each group, they will occur in alphabetic order, so M then O then Y.  So it may be  better to use codes that will follow a natural sequence - this means when you want to paste output into a table you don't need to fiddle about with it.



Another thing to note is that if you have a program that treats codes as alphabetic, then if you have, say, 20 subjects, and you sort them, they will come out in the order: S1, S10, S11, S12, S13, S14, S15, S16, S17, S18, S19, S2, S20, S3, S4, S5, S6, S7, S8, S9. This mildly irritating feature can be avoided if you ensure all codes are the same length, e.g. S01, S02, and so on.



On the other hand, if you are generating raw data files that you want to process automatically through some analysis package, make sure you have codes that can be easily read in a loop. It's much easier to tell a program to sequentially analyse files beginning with S and ending in numbers 1 to 20, than it is to type in each subject code separately.



And if you are going to analyse a whole set of files using an automated procedure, use a logical folder structure to organise your files. I've been stymied by finding that someone has carefully organised data files so that all the data for one child on various tasks are in one folder, and these folders are then within other folders that group them by age. I prefer it if all the files that are to be analysed together are kept together: provided the file-naming system is well-constructed, there should not be any chance of confusing who is who, and you can then point the analysis program just to one relevant folder, without a lot of if statements.




2. Label your variables in a consistent and intuitive fashion that will work across platforms


If you are going to end up analysing your results in SPSS, start out with variable names that SPSS will accept - i.e. no blanks, leading numbers or prohibited characters should be included. Think ahead to the paper you plan to write about the results and consider the variable names you will use there. I seldom obey my own advice here, but it's a common source of irritation to reviewers if you are inconsistent in how you refer to a variable. Much better to start as you mean to go on as far as is possible.




3. Use 'freeze panes' in Excel


This is about as basic as it gets, but I'm surprised at how many people don't know about it. In Excel, when you scroll down or across your file, the variable names or subject IDs scroll off the screen. If you place your cursor in the cell just below the variable names and just to the right of the subject IDs (i.e. the first cell of data), and select View|Freeze panes, the rows and columns above the current cell will stay put when you scroll. If you get it wrong, you can always unfreeze.



There's a rather clunky method that lets you freeze panes in SPSS, which can be useful if you want to see subject IDs while scrolled over to the right: see here for instructions


4. Keep an explanatory list of your variables


In SPSS, the 'labels' field can be useful for keeping a record of what the variable is, but it is limited in length and sometimes more detail is needed. It's worth keeping a data coding file which lists all variables and gives a brief description of what they are, what missing value codes are, and so on. This is absolutely critical if you plan to deposit data in an archive for sharing. It's good practice to work as if that is going to be the case.




5. Use one big file, rather than lots of little files, and hide variables that you aren't currently using




If you have a large dataset, it's tempting to break it up to make it more manageable. You may have hundreds of variables to contend with. You may therefore be tempted to pull out variables of current interest and store in a separate file. The problem is that if you do that, it's easy to lose track of where you are.



Suppose you have a giant master file, and you select a few variables to make a new file, and then in the new file you find an error. You then need to correct it in both files, which is tedious - so tedious that you may not bother and will then end up with different versions and be unsure which is correct.



Also, you may want to look at relationships between the variables you have extracted and other variables in the master file. This involves more fiddling with files, which is a good way of generating errors, especially if you use cut and paste.  So my advice is stick with one master file, which is scrupulously labelled with a version number when you update it. You can avoid the 'too much data' problem by just hiding bits of file that aren't currently in use.



In Excel, it's simple to just hide rows or columns that you aren't using. You just select the columns you want to hide and select View|Hide. If you want to see them again, you select the columns adjacent to the hidden columns and select View|Unhide.



You can do a similar thing in SPSS by defining Variable Sets. It's a bit more fiddly than the Excel operation, but once you have defined a variable set, it is saved with the file and you can reselect it very easily. Instructions for doing this are here.



This website, incidentally, is a treasure trove of useful advice, including instructions on  how to produce APA formatted tables from SPSS output.




6. Never name a file with the suffix 'final' and always back up key data


It's just tempting fate to call a file 'final'. You will end up with files called 'final final' or 'really final' or 'final v.10'. Better to use dates to identify the most recent version.



The back-up advice is blindingly obvious but even the most seasoned of us still forgets to do it. If you've put in several days' work on something, you need to have it stored safely in case your computer dies or gets stolen.


7. Look at your data


Before rushing into an analysis, it is important to plot your data. This can be a good way of picking up gremlins in the dataset, such as values which are out of range. For instance, if you have raw scores and scaled scores on a variable, plot one vs the other in a scatterplot - depending on whether there is age variation in the sample, scores should either fall on a straight line, or at least cluster around it.

You should also check whether variables are normally distributed, and if not consider how to deal with this if your analysis assumes normality. Andy Field's textbook Discovering Statistics Using SPSS gives helpful advice on this general topic (and many more!).


8. Keep a log of your analysis


I find it helpful to think through what I want to do, then make a list of the analyses and outputs that I need and work through them systematically. In practice, things seldom go smoothly. You may find that a subject's file is missing, or corrupted, or that data need transforming in some way. It's traditional to work with a lab book in which such things are recorded, though I prefer to do this electronically when at the analysis stage, by just keeping a Word document open, and making a note of everything as I go along, under the relevant date.



In this log I note the names of the files I've created and their location and what they do. This really is necessary if you are to avoid a future time when you have to wade through numerous versions of numerous files trying to find the one you can only dimly remember creating.



I also record problems in the log. For instance, suppose you have a task that was wrongly administered in a couple of cases so the data will have to be excluded. The log is where you record the date at which this was noted, which data were affected and what action was taken. If you don't do this, you may well find that you, or someone else, comes back to the dataset at a later time and cannot make sense of it. Or, as I have done all too often, spends a morning discovering the same problem that was already found months previously.


9. Use scripting in SPSS


The best advice of all is to keep a script of your analysis if you are working in SPSS. Even if you know nothing about scripting, this is very easy to do. Set up your analysis using the menu, and instead of hitting OK, you hit Paste. This opens a script window showing the script-version of the commands you have selected. You can then select all or part of the script and run it by hitting the big green arrow at the top of the script window. If you then run another analysis, and again hit Paste, the new syntax will be appended at the bottom of the script.



There are four advantages to doing things this way:


  • You can save the script and thus have a permanent record of the analysis you have carried out. This complements the log you are keeping (and you can save its name in the log).

  • You can annotate the script. Any text you type in that begins with an asterisk and ends with a full stop is treated as a comment. You can use this to remind yourself of what the analysis does.

  • You can come back and re-run the analysis. Suppose you find that you had an error in your dataset and you had to correct one person's data. Instead of having to laboriously reconstruct the whole analysis, you just  re-run the script.

  • This is a good way to learn about scripting. A lot can be picked up by just taking the auto-generated script as a model and tweaking things like the variables that are analysed. If you want to do a parallel analysis on several variables, it is much easier to copy and paste the relevant section of a script and change one or two variable names than to go through a menu.



10. Check all analyses before publishing


It is really important to check all your analyses before you submit a paper. Always go through a paper and make sure that all reported tables and analysis are reproducible. It is amazing how often you re-run an analysis and things come out differently. It can seem sometimes that a malign spirit inhabits your computer and is just teasing you. Even if the  differences are not serious, they can still be a source of worry. In my experience, they often have to do with things like forgetting to select the correct subset of participants for a specific analysis - if, - for instance, there are exclusionary criteria. Or a missing data code may have been  inadvertently been treated as data. In the worst case you may find you cut and pasted something into a file forgetting that the file had been sorted in a different order. And sometimes, just sometimes, both Excel and SPSS files can get corrupted. It can be useful to have data in both formats for an overall consistency check on things like mean values.



This is where SPSS scripting comes into its own. The whole business of re-running the analyses becomes much more tractable with a script. Furthermore, in a final check, you can further annotate the script, noting which table in the paper corresponds to a particular output and so have a nice, clear account of what you did to refer back to.




Wednesday, April 16, 2014

Near-Term Human Extinction

Global Warming and Feedbacks

Is there a mechanism that could make humanity go extinct in the not-too-distant future, i.e. within a handful of decades?

Most people will be aware that emissions due to human activity are causing global warming, as illustrated by the arrow marked 1 in the image on the left. Global warming can cause changes to the land, to vegetation and to the weather. This can result in wildfires that can in turn cause emissions, thus closing the loop and forming a self-reinforcing cycle that progressively makes things worse.

Furthermore, less forests and soil carbon also constitute a decrease in carbon sinks, resulting in carbon that would otherwise have been absorbed by such sinks to instead remain in the atmosphere, thus causing more global warming, as illustrated by the additional downward arrow in the image on the right. In conclusion, there are a number of processes at work that can all reinforce the impact of global warming.

Emissions can also contribute more directly to land degradation, to changes in vegetation and to more extreme weather, as indicated by the additional arrow pointing upward in the image on the right. A recent study by Yuan Wang et al. found that aerosols formed by human activities from fast-growing Asian economies can cause more extreme weather, making storms along the Pacific storm track deeper, stronger, and more intense, while increasing precipitation and poleward heat transport.

Accelerated Warming in the Arctic

Similar developments appear to be taking place over the North Atlantic. Huge pollution clouds from North America are moving over the North Atlantic as the Earth spins. In addition, the Gulf Stream carries ever warmer water into the Arctic Ocean. As the image below shows, sea surface temperature anomalies at the highest end of the scale (8 degrees Celsius) are visible off the coast of North America, streching out all the way into the Arctic Ocean.


As said, feedbacks as are making the situation progressively worse. Feedback loops are causing warming in the Arctic to accelerate. Warming in the Arctic is accelerating with the demise of the snow and ice cover in the Arctic, and this is only feedback #1 out out many feedbacks that are hitting the Arctic, as described in an earlier post. As the temperature difference between the equator and the Arctic decreases, the Jet Stream is changing, making it easier for cold air to move out of the Arctic and for warm air from lower latitudes to move in (feedback #10).


Abrupt Climate Change leading to Extinction at Massive Scale

The danger is that, as temperatures over the Arctic Ocean warm up further and as the Gulf Stream carries ever warmer water into the Arctic Ocean, large quantitities of methane will erupt abruptly from the seafloor of the Arctic Ocean, adding a third kind of warming, runaway warming resulting in abrupt climate change, and leading to mass death, destruction and extiction of species including humans.

Persistence of such a progression makes it inevitable that the rest of Earth will follow the huge temperature rises in the Arctic. Massive wildfires will first ignite across higher latitudes, adding further greenhouse gas emissions and causing large deposits of soot on the remaining snow and ice on Earth, with a huge veil of methane eventually spreading around the globe. The poster below, from an earlier post, illustrates the danger.

[ click on image to enlarge - note that this is a 1.8 MB file that may take some time to fully load ]
Views by Contributors

How likely is it that the above mechanism will cause human extinction within the next few decades? What views do the various contributors to the Arctic-news blog have on this?

Guy McPherson has long argued that, given the strengths of the combined feedbacks and given the lack of political will to take action, near-term human extinction is virtually inevitable.

In the video below, Paul Beckwith responds to the question: Can climate change cause human extinction?


Further contributors are invited to have their views added to this post as well. While many contributors may largely share Paul Beckwith's comments, it's important to highlight that contributors each have their own views, and this extends to their preference for a specific plan of action.

Geo-engineering

One of the more controversial issues is the use of geo-engineering. Guy McPherson doesn't believe geo-engineering will be successful. In the video below, Paul Beckwith gives his (more positive) views on this.


I must admit that the lack of political will to act is rather depressing, especially given the huge challenges ahead. So, I can understand that this can make some of us pessimistic at times. Nonetheless, I am an optimist at heart and I am convinced that we can get it right by giving more support to a Climate Plan that is both comprehensive and effective, as discussed at ClimatePlan.blogspot.com





Monday, April 14, 2014

M4.5 Earthquake hits Arctic Ocean

An earthquake with a magnitude of 4.5 on the Richter scale hit the Arctic Ocean on April 13, 2014, at 02:12:19 UTC at a depth of 10.00 km (6.21 mi).


The epicenter of the quake is located right on the faultline that crosses the Arctic Ocean, at 86.687°N 45.393°E, some 800 km north of Franz Josef Land.

Earthquakes at this location are very worrying, as they can destabilize hydrates contained in the sediment under the seafloor of the Arctic Ocean. Furthermore, one earthquake can trigger further earthquakes, especially at locations closeby on the same faultline.




Related

- Earthquakes in the Arctic Ocean
http://arctic-news.blogspot.com/2014/04/earthquakes-in-the-arctic-ocean.html

- Methane, Faults and Sea Ice
http://arctic-news.blogspot.com/2013/11/methane-faults-and-sea-ice.html

- Norwegian Sea hit by 4.6M Earthquake
http://arctic-news.blogspot.com/2013/11/norwegian-sea-hit-by-46m-earthquake.html

- Greenland Sea hit by M5.3 Earthquake
http://arctic-news.blogspot.com/2013/10/greenland-sea-hit-by-m53-earthquake.html

- Earthquake hits waters off Japan
http://arctic-news.blogspot.com/2013/10/earthquake-hits-waters-off-japan.html

- Earthquake hits Laptev Sea
http://arctic-news.blogspot.com/2013/09/earthquake-hits-laptev-sea.html

- Methane Release caused by Earthquakes
http://arctic-news.blogspot.com/2013/09/methane-release-caused-by-earthquakes.html

- Earthquake M6.7 hits Sea of Okhotsk
http://methane-hydrates.blogspot.com/2013/10/earthquake-m67-hits-sea-of-okhotsk.html

- Sea of Okhotsk
http://methane-hydrates.blogspot.com/2013/06/sea-of-okhotsk.html

- Seismic activity
http://arctic-news.blogspot.com/p/seismic-activity.html

- Climate Plan
http://climateplan.blogspot.com



Saturday, April 12, 2014

WeSpeechies: A meeting point on Twitter








As an avid Twitter user, I'm always interested in new
developments in social media, and so I was intrigued when Caroline Bowen (@speech_woman) and Bronwyn Hemsley
(@bronwynhemsley) invited me to curate a session of @WeSpeechies for a week.


I said yes immediately, though I had no real idea (and still
have no real idea) of what I was getting myself into. But I knew that Caroline
had done an enormous amount to encourage 'Speechies' (i.e., Speech and Language
Therapists in the UK/Speech-Language Pathologists elsewhere) to use the
internet. In 1998, she started a web-based resource: this is a mine of useful information, including links to assessments, interventions and
evidence-based information.



I'm not a speechie myself –  I'm a full-time researcher with a Principal Research
Fellowship from the Wellcome Trust and my background is neuropsychology -  
but I've always worked closely with the profession, because of my
interest in children's communication impairments. So it's great to have the
opportunity to interact with those who work at the coalface, and @WeSpeechies
seems like a great idea.



But how does it work? Well, there's a description here.



In brief, the idea is that the Twitter handle @wespeechies
is taken over by someone – the 'curator' – for a week, with the idea that they
can foster interesting exchanges on Twitter. What's more, the interactions can be preserved: this can be helped if those interacting
with @wespeechies remember to add the hashtag #WeSpeechies to their tweets.This way we can build an archive of useful and interesting interactions.


Now, of course, most of us are not glued to Twitter all day,
even though we may give that impression, and there can be difficulties in
interacting across time zones. As curator,
I plan to check in a couple of times every day during the week to respond to tweets, but Caroline and Bronwyn wanted also to ensure that there is an
opportunity for some live chat. They therefore include in the course of the
week a "Tuesday Chat", which involves me chairing a Q&A session. Caroline and Bronwyn have kindly
given me an easy topic for my first attempt, namely Apprehensive Academics on
Twitter – inspired by this blogpost.


I'm going to do this at 8 to 9 in the morning on Tuesday 15th April 2014 on
British Standard Time. This means that the live chat should appeal to night
owls in North America, and larks in UK and Europe, whereas for those in
Australasia it will be afternoon or early evening.



If you'd like to take part, please feel free to respond to
any message from @wespeechies, and remember to include #WeSpeechies in your
message. I've generated some questions to get the ball rolling; if you want to
answer one of these, please make it clear which one by including, for instance,
A1, A2, A3 etc at the start of your Tweet.



Q1 What makes for an effective/ineffective tweet?
#WeSpeechies








Q2 Have you got any tips for attracting followers?
#WeSpeechies








Q3 Are there downsides to Twitter? #WeSpeechies 



Q4 What unexpected benefits of Twitter have you found?  #WeSpeechies








Q5 Does your employer have an issue or policy on staff being
on Twitter, that you know about? 
#WeSpeechies


Please note that the idea of #WeSpeechies is to engage and
connect with those who work as SALTs/SLPs or who have shared interests in problems affecting communication and/or swallowing. You don't need to be an expert – on
the contrary, part of the fun of the exercise is that we can all share
experiences and maybe learn something new. The hope is that, if you take
part, you may find new contacts around the globe: people with shared interests
who can make you feel more of a world-wide community.



A final note of warning: WeSpeechies does not encourage advertisers, spammers or trolls. It is
not the place to try and sell or endorse a product. Anyone who does not
abide by the basic @WeSpeechies guidelines will be warned and then blocked if
the advertising or unsuitable promo Tweets continue.



















from geek-and-poke.com



If you are interested in speechie issues, I do hope you will participate by following @WeSpeechies. I'll be
taking over the twitter handle on Sunday 13th April for a week, so look forward to
meeting you there!



P.S. 15th April 2014

The Live Chat was fun, if somewhat frenetic.

If you missed it, you can see the tweets collated here: