By Frederic Maps on January 13, 2012 1:46 PM
|1 Comment
I've just finished yesterday (just on time, as usual!) grading the final assignment of undergrads from the "Université du Québec à Rimouski" for a fall session class entitled "Functioning of Marine Ecosystems".
And yesterday something stroke me. When I was producing a report (not so long ago) supposed to describe the patterns and processes prevailing in a marine ecosystem, I had David Attenborough's voice in my head chanting "The sun shines relentlessly over the blue sea, providing a tremendous amount of energy capable of moving water masses and make microscopic life bloom..."
But I think that my students heard a David Suzuki of some sort warning "There is an urgent need to describe and understand the current state of the marine ecosystem in order to face the impacts of global change and the ever increasing human pressure over the ocean..."
The vast majority of those 20 pages reports supposed to describe
some specific marine ecosystems (The Gulf of Maine, the Baltic etc) were presented that way, to the point where some almost lost sight of the purpose of the assignment and spent more pages listing the current threats to their systems than characterizing its state and dynamics.
During the past session we had a variety of lectures and discussions, they did several presentations on various relevant topics. I did my best to put forth a balanced approach, but these students definitely learned ecology in a context radically different from what prevailed until the end of the last century. Canadian Conservative Ministers of natural resources will have to learn living with those new "radicals"!
By Pam Moriarty on November 18, 2011 5:34 PM
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First off, let me introduce myself.I'm Pam, I've been a GMRI intern for
the last 5 months or so and have been lucky enough to be part of the salmon
team here.It's been a great
experience and I've definitely learned a lot!
There's a couple of salmon-related
projects going on at GMRI, I've been involved with work studying Atlantic
salmon migration in the Gulf of Maine.In the Gulf of Maine, salmon begin their migration when they enter the
marine environment.This initial
migration phase occurs as they move through the Gulf of Maine to the coast of
Nova Scotia by Halifax (they then continue all the way up to Greenland).However, we don't know where in the
Gulf of Maine the salmon are moving through, how they're finding their way
through or how the variability in the Gulf of Maine physical environment
(currents and temperatures) affects them.I've spent the last several months trying to address these questions using
what's known as "individual-based modeling" (IBM).
IBMs let us simulate individual fish.We can give the fish different sets of rules
to define their behavior.This is
neat because it lets us experiment with different orientation methods to see what
methods might be plausible and lets us simulate the path an individual fish
follows through the Gulf of Maine.Then by using physical conditions from different years, we can see how
these paths change due to differences in temperatures and currents.
This figure shows simulated tracks for
fish- each red line is a different fish. For this figure, the fish were
instructed to swim in the direction the current was flowing.
As it turns out, the salmon are affected
by interannual variability in their environment.In general, stronger currents result in fewer salmon
successfully navigating their way through the Gulf of Maine.However, the degree to which changes in
currents affect salmon depends on how salmon orient for migration.If salmon use directed swimming (know
the direction they want to go and try to swim in that direction), then changes
in currents do not have that large of an impact.However, if salmon use other behaviors (such as using
temperatures and/or currents to navigate), then changes in currents do have a
larger impact.Also, while we have
no way right now of concluding what behavior salmon do use to orient, we can rule out a
couple of possibilities.Based on
the lack of success (i.e. no fish make it to Halifax), we know that the salmon
aren't passively drifting and aren't simply swimming in the opposite direction
of the currents.
By Sigrid Lehuta on September 13, 2011 4:00 AM
|1 Comment
So I guess this is the day, I launch into the lab blog! First
let me introduce myself. My name is Sigrid, I am a post-doc freshly arrived in
the lab last February (so "fresh" refers more to the weather at the time than
to the duration of my stay). I am a modeler, defended my phD last November
dealing with the assessment of impacts of marine protected areas on the anchovy
fishery in the Bay of Biscay. I am currently working on the interaction between
herring and lobster in the Gulf of Maine. Last thing you need to know and you
may have already noticed, I am French, so please forgive my potential mistakes
in English. Voila! Everything's said, we can go.
I guess it's good form to start with a copepod joke...
OK copepod joke: done
More seriously, I had the opportunity to travel to Seattle
last week to attend the 141th conference of the American Fisheries Society
titled "New frontiers in fisheries management and ecology: leading the way in a
changing world". This was an exciting event I wanted to share: 4 days, 94
symposia and about 4000 participants among them some of the most famous
fisheries scientists, I felt in the Hollywood of fishery science! Consequently
the organization comity was forced to move the plenary sessions to the
Paramount Theater, a magnificent performing arts venue built in 1929 and that
hosted famous names such as Madonna for her first concert and of course the best of the Seattle grunge stage such as Soundgarden and Nirvana.
There was thus a big pressure on the plenary speakers who certainly
made it by reminding us how Fisheries science rocks! The essence
of the talks pretty much fits GMRI's vision, see yourself:
Dr. Randall Peterman from British Columbia's Simon Fraser
University gave a talk titled An optimistic view of
challenges facing fisheries scientists and managers. Heemphasized the need for
multidisciplinary approaches (from ecologists to social scientists) to address
the complex interactions between human and natural systems. He also pointed out
the necessary communication between scientists and managers that would require the
acquisition of new skills on both sides to address the question of risk
assessment and risk management conjointly. He
listed his reasons to be optimistic concerning the future of fisheries, among
others, the rising development of certification and sustainable seafood labels,
the increasing inclusion of uncertainty at every levels of the management
decision process, and the potential represented by young scientists
increasingly trained in all aspects of the field (ecology, physics, economics,
communication, quantitative methods).
Dr. Robert Lackey retired from Oregon State University then dissected
the underlying implications of this 141th AFS conference theme: leading the way
in a changing world. He stressed the necessity to look forward to the problems
that fisheries will face in the next years giving the important changes we
experience and will experience in climate and economics. He said that "there is
no "good all days" and there won't be any in the future". He discussed the role
of scientists in management decision accenting their duty of neutrality and the
risk of scientist corruption. He finished by emphasizing the need to "reject
pessimism and optimism and embrace realism!".
Finally Dr. Jesse Trushenski from Southern Illinois
University - Carbondale gave a metaphoric talk titled The Ecology of Fisheries Education -- Are We
Adequately Preparing the Next Cohorts for a Field in Flux? cleverly
transposing ecological concepts to principles in the education of young
scientists. She stressed the need for specialized generalists able to adapt quickly
especially to work with imperfect data. She also emphasized the need to keep
students connected to the field, ready to "get dirty! " and to recognize than
science is "half brain, half gut! ". She promoted the development of a balanced
r/K strategy as a parallel with selection theories that would produce high
quality students, in reasonable number given the limited professional
opportunities but with good adaptive skills to face the rapid changes
experienced in our field.
To get some taste of the best I grabbed from the symposia,
have a look at the figure below. Aside from the conference I get the chance to
see fish flying... at pike place market, chipmunks eating grapes on the sides of
Mont Rainier and marine scientists excited about touching sea urchins and starfish at
Seattle Aquarium touch tank!
By Jane Carpenter on August 10, 2011 7:39 PM
|1 Comment
So I realize that my 10th and final week at GMRI is a bit late to be writing my first EML blog post, but as they say, better late than never!
To briefly introduce myself, I'm Jane, the ecosystem modeling lab summer intern. My summer project has been to work with the "compupod" model, trying to model the biogeographical limits of four copepod species: three Calanus species, as well as Pseudocalanus newmani. It's been a fun journey (though not without its trials and tribulations), and I've learned a lot along the way.
Having never programmed before this summer, at the beginning I faced some frustration while working with Matlab. Andy and Nick may have as well when I asked them questions like, "So how do I limit the latitude and longitude ranges again?" and "Why are my figures coming up as lime green boxes?" Eventually, however, I got the hang of Matlab and learned how to create pretty maps such as this:
(This figure shows the predicted lifetime egg production for Calanus finmarchicus).
My learning experience this summer has not been limited to expanding my knowledge about copepods and improving my Matlab skills, however. I've gained a better understanding of the process of conducting scientific research, and of what it's like to work in a research environment. Flexibility is key; if your project starts to lead you in a different direction, exploring it instead of sticking to your intended plan may lead to some interesting discoveries. I also appreciate the importance of persisting in spite of roadblocks. It was discouraging when my model runs led to unrealistic predictions...but I realized that revisions are an inevitable part of the process.
I've also experienced what it is like to work with intelligent, engaged, hilarious people, not just in science but in every department at GMRI. I have to say, it has set the bar high for my future jobs.
I am sad to see the summer come to an end, but will end this post on a happy note; since today we realized that "copepod jokes" returns zero hits on Google (shocking, right?!), here is the best one I could come up with:
Why didn't the bank let the copepod withdraw money from his
account?
They knew he was a Pseudocalanus.
And when I said it's the best copepod joke I could come up with, I really meant the only one...but don't worry, the lab is working on it. :)
By Nick Record on July 20, 2011 6:47 PM
|No Comments
Hmmm...
(Mathematicians) (Oceanographers) sin θ ?
Something about a "sine wave"?
I'm sure there's a punchline there somewhere.
At any rate, I recently returned from a great workshop where a subset of mathematicians and a subset of oceanographers intersected in the same pool. It took place at the Mathematical Biosciences Institute at Ohio State. The mix of people and perspectives was great, and the atmosphere was one of learning and brainstorming. There is certainly a need for more integration of these two fields.
The talks spanned a range of topics, ranging from mathy to oceany. Many of the presentations were live-streamed, and can be downloaded here. My talk, "Toward a Grand Unified Theory of Copepods" is posted here: Before you click, be warned: it's nearly an hour long. Make certain you have some time--you might not be able to tear yourself away.
By Dom Fitzpatrick on July 15, 2011 6:22 PM
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After being in the ecosystems modeling lab for
over a month now I have (believe it or not) started to learn a few things.
As I'm new to the blog I guess I should
introduce myself a bit.My name is
Dom and I graduated from Bowdoin College in 2009.I am just starting a MS in Oceanography at the University of
Maine and will be doing most of my study/work remotely from the EML.In undergrad I majored in physics with
a minor in math and somehow found myself at GMRI.I am new to ecology and ecosystem studies. I have taken
biology courses in the past, but never really studied anything about fisheries
before now.Here are some thoughts
I had piling up since I've started...
Like Nick got into in a recent post, it has
been interesting to see the degree of uncertainty so far.I knew the ocean was relatively
unexplored and is known as a "mysterious frontier" (at least to me), but some
of the unknowns caught me by surprise.Things like fish mortality rates and egg production rates are very
difficult to find.Migration
patterns for species are modeled, but it seems to change from year to year,
especially as the environment changes... so how useful are our models. People are
tagging fish, weighing samples, measuring lengths among other data collection
methods, but even with all this data we still have to extrapolate and fill in
blanks.Maybe this makes
everything more exciting...
Going along with that idea is the significance
of assumptions.Some how we have
to use what we have and try to make predictions."We don't know it?... Let's assume this for now and we'll go
from there..."
The data and its use have been interesting to
me so far. I should have seen this coming, but trying to make predictions with
the data we have is a tough task.When you think about predicting the dynamics of a populations of herring
in the GOM, consider the circumstances: there is only data from the last 20
years, individuals could be 10, 12 or even 20 years old, they can swim in and
out of this region at any point, stocks can take decades to shift and cycle...
It just seems as though there are so many variables that it is impossible to
know where to start.
Data is collection is difficult and data
collected is difficult to work with.External conditions can create holes (i.e. a study can miss a
measurement of copepod abundance during a given winter in the GOM).
From what I have seen so far it seems that
everyone is trying their best with the resources and information we have
available to us.I guess this is
all we can do.It's easy to see
how these obstacles can seem overwhelming.I think the idea is to make sure we have short term,
attainable goals and remind ourselves of the big picture from time to
time.It is undeniable that
everything we are working on is important and relevant.Keeping this in mind is key.
This is what I have picked up on so far.It may seem a little dreary, but I
think it also excites people... I'm excited... I think.
By Frederic Maps on June 3, 2011 3:58 PM
|No Comments
I've just opened an email form a colleague informing us that from today onward, the National Academies Press will offer its electronic books and reports for free. They even provided the code to embed in anybody's webpage. It's neat, as you can see by yourself. Go there and browse the catalog. There's definitely something for you.
By Frederic Maps on April 29, 2011 4:11 AM
|1 Comment
Last week I attended in
UQAR a long presentation given by a climate modeler from the OURANOS consortium
on regional climatology and adaptation to climate change, based in Montréal, Québec.
I picked among the wealth of information provided a survival kit to use in any
occasion you face a so-called skeptic. They are inconveniently widespread now,
even among your family, friends or neighbors, the federal government, and worse,
they are spreading outside of the US into Canada as I'm writing this blog entry...
So, skeptics cherish a
handful of "arguments", which are not (only) bad or misunderstood science, but
are essentially outdated science, and when you'll face it you'll have to debunk
it! The skillful skeptic will probably not deny the global increase in atmospheric
CO2 since the beginning of industrialization (Documented first by
Callendar in 1938), as Andy recently pointed out, but rather deny its impacts
on climate through a short list of arguments, some of them being:
"Climate changes are forced by the sun (not my
SUV)"
This argument is
incomplete and out of date. This was a legitimate scientific hypothesis formed
by Milankovic in the 40's. He thought that the intricate interplay of the
precession, obliquity and eccentricity of the earth altered the radiative forcing from the
sun, and thus the climate. However as early as the 70's with the help of the first ice cores
(some made by Milankovic himself...), it was proven that this effect would essentially modify
the seasonality of the sun forcing, and not the total quantity of radiation reaching
the earth which is what is important in the radiative balance of the planet. Moreover it could not explain a number of fast historical climate changes
events, nor the warming trend of the last 30 years.
The more subtle skeptic will try to ensnare you in some apparently complex issues like:
"H2O vapor already blocks infrared
wavelengths, so an increase in CO2 (by my SUV) won't change the
earth's radiative balance"
This argument is of the
oversimplified type, and is actually wrong. To better get the importance of infrared absorption by gases, please refer
to this pages for a quick introduction of radiative balance of the planet and
greenhouse effect. Basically, H2O doesn't absorb at all the infrared
wavelengths that CO2 can absorb. So despite water vapor being
overwhelmingly abundant, there is still room for an increase in heat in the
atmosphere solely due to increased infrared absorption by increased atmospheric
CO2. Plass realized this in the early 50's after a careful study of
infrared wavelengths absorption by water vapor and other gases. He published as
early as 1956 all of the major figures now confirmed by measurements and advanced
numerical models in the most recent IPCC science reports: temperature increase
by year 2000, temperature increase if doubling of CO2, etc. Plus, as Andy has just shown, an increase in heat due to CO2 will lead to an increase in water vapor, ad hence a positive (more warming) feedback...
And about feedback and climate
numerical models, what about:
"Models are oversimplified, don't take in to
account water vapor (!) and overlook feedback."
Well nowadays climate
models are FAR from simple, and beyond their physical and numerical
structure, the way they are used presently (ensemble approach, with
powerful statistical methods to get meaningful confidence interval etc.) are
far more advanced than usually thought. There is a widespread misconception equating
the problem of predicting weather (a chaotic monster) and climate (the
statistical resultant of many weather events)...
For water vapor, it was
first modeled in 1967 by Manabe & Wetherald, and there is simply NO modern
model that overlook it. Finally, most climate models now incorporate feedback
from land (including vegetation, wild fires, volcanoes etc.), the ocean and the
cryosphere (ice).
I leave you with a very
nice animation presenting the current state-of-the-art climate modeling. This
animation was made for the Pierre-Simon Laplace Institute of France, so the
comments are in French, but I can assure you it's a great piece of climate modeling for
the layman!