Atmospheric Dynamics Absorbing Ground Emissions. Wildfires On The Ground and Smoke Up In The Sky (by Diego Fdez-Sevilla PhD)

Atmospheric Dynamics Absorbing Ground Emissions. Wildfires On The Ground and Smoke Up In The Sky (by Diego Fdez-Sevilla PhD)

CV english and españolResumeInterdisciplinary Skills applied in the line of research presented.- Index for all analyses published. – Shares and Feedback at LinkedIn. DOIs for those publications mentioned can be found at the Framework and Timeline Page.

“Atmospheric Dynamics Absorbing Ground Emissions. Wildfires On The Ground and Smoke Up In The Sky (by Diego Fdez-Sevilla PhD) July 2015 DOI: 10.13140/RG.2.2.21332.65923 Project: Filling In/Finding Out Gaps Around in Environmental Sciences. “

Hundreds of wildfires are burning across Northwest Canada, particularly in British Columbia and Saskatchewan. The fires have spread smoke southward, across the U.S., causing air quality to deteriorate, and producing reddish sunsets from the Midwest to the Southeast.

The fires have been so intense and so numerous that Canada has appealed for international assistance, with firefighters coming to the country from as far away as Australia and Mexico.

According to the Canadian Interagency Forest Fire Centre, more than 4,500 individual fires have already burned, which is an unusually high figure so early in the year. A total of 2.7 million acres have already gone up in smoke. Wildfires have also been a major problem in Alaska.

A National Oceanic and Atmospheric Administration (NOAA) satellite captured these circulations in a Canadian wildfire smoke plume, which was crossing the border on Friday morning over Montana. The National Weather Service office in Glasgow, Montana, posted images on Facebook. (Wildfire smoke, July 10, 2015. more here and here)

Circulations in wildfire smoke spotted by satellite on July 10, 2015. Image NOAA.

Atmospheric circulation

As air flows throughout the atmosphere atmospheric waves are often generated describing the dynamic behaviour of a fluid. Accordingly, those patterns are quite similar to ripples in a pond or eddies in a river. But furthermore, if the flow is laminar (like straight hair) or turbulent (curly hair), it can also give us indirect information about the thermal conditions (stability, etc) and homogeneity in the composition (water vapour… ) of the air. And changes in those visual patterns usually help to locate “factors” generating weather events (e.g. weather fronts, cyclonic circulation and adiabatic processes). Those can be when two or more different (thermally or water content dry/humid) masses of air get in contact or even when orographic features interfere with tropospheric circulation inducing changes in those air masses due to e.g. changes in pressure and thermal gradients in altitude.

Some of those waves are visible thanks to the condensation of water but most often those waves are invisible. However, similarly as with experiments in a wind tunnel aimed to observe aerodynamic behaviours, here the smoke from fires allows us to see patterns in atmospheric circulation which we might not see otherwise.

In particular, in the following image from Aqua Satellite, we can see how the mass of air being generated by the fires interact with the Jet Stream at 250 hPa moving West to East over the North American continent and into the Atlantic Ocean.

Canadian fires 10 July Aqua Modis

Image is from the Aqua/MODIS satellite, taken on July 10th. I added the location of wildfires which are represented by the red dots.

Jet stream 10 July 2015

Wind Speed at 250 hPa, Jet Stream, on 10th July 2015. Data from Nullschool and GFS/NCEP.

The 10th of July, the same day that the previous satellite images caught the smoke from Canadian wildfires in atmospheric circulation, I was looking at the state of the overheated atmosphere in Southern Europe. Among other resources I was looking at the real time images being broadcast by the International Space Station (there is a link and video streaming on the right side of this blog). During its fly over the North Atlantic (from west to east) the ISS had operational the camera facing backwards. The next image shows the state of the atmosphere over the North west Atlantic where we can see the grey trail of smoke getting spread in a wide whirlpool at stratospheric circulation.

Black smoke from Canadian wildfires reach stratospheric circulation.

 Interferences with the Jet Stream

I believe that the previous images offer a vivid illustration of how easily plumes of air being generated over land, containing diverse composition of gases and aerosols (in this case COx and ashes from the combustion of wood), get introduced high in atmospheric circulation.

In the actual times, the relevance of such assessment is a matter of open discussion. Some points of view defend that the atmosphere can take almost everything that activities overland might generate without the patterns followed in global atmospheric circulation suffering any major alteration over time. Personally, based on my limited knowledge, I do not see it as an accurate point of view.

Actually, in climatology, one point of view adopted by many is based on that natural variability force us to have to consider periods of at least 30 years in order to define changes of global climate relevance. Such posture allows to consider extreme and unseasonal weather events as part of natural variability, and they will only become relevant if they persist in time over a 30 years period.

So, this posture opens for me some questions.

In environmental science, the scientific approaches applied to analyse patterns and settle laws, are based on repetition. Accordingly, the link between cause and causation is only proved when it is allowed its replicability, either by artificial means (experiments) or by observation. So it is prioritised the number of repetitions over any other approach. And the repetitions have to describe the same events following the same steps in the same chronological order.

In a past scientific project I led a study looking into the aerodynamic behaviour of pollen grains of different types. Subsequently I performed several experiments in a controlled environment (wind tunnel). Having control over the environment (wind speed, temperature and humidity) allowed me to replicate several times specific conditions under which to capture those particles when they were airborne. That was necessary to demonstrate that pollen types with different morphology and size behave differently as a result of their aerodynamic characteristics.

In climatology, however, the environment in which we observe events happening has not controlled parameters. Therefore, it is a challenge to find climatic events which can be profiled as “similar” in order to be compared as repetitions defining a pattern. But, even understanding such dilemma, here is where I see that there are some limitations in the scientific approach applied due to its narrow capabilities.

In one hand, narrow capabilities derived from the conflict between the concept of natural variability and replicability.

Both terms play opposite roles in environmental developments. One introduces the unsettling feeling of unpredictable constant changes as a natural pattern meanwhile the other looks for settling rules dictating predictable outcomes. And yet, they both share in common the fact that for something to happen, there must be a confluence of many variables in the right order and proportionality. So even the existence of a single event, as much rare or brief as it can be, is the expression of a “real” scenario. And since it has happen and it has been observed, it is not longer a “possibility”.

Once the reality of this scenario to exist has been proven, it becomes a matter of concern to evaluate what is already different that allows for such scenario to exist. Just to use a similar idea. If NASA designs a protocol to launch a vehicle and finds the existence of one single unpredicted “glitch” at any time when following trials, this carries the concept of “reality” for unpredicted events to happen. In another words, the system is “unstable”.

From this analytical approach, one single event, which is not enough to represent a statistical value, becomes the representation of a scenario only possible by the confluence of multi-variables. Therefore, its own existence makes it statistically representative of a statistically meaningful number of variables, magnitudes of those and location.

Venice Event Tornado by Diego fdez-Sevilla

Tornado-producing severe thunderstorm in northern Italy. July 8th, 2015

In other hand, when we look at climatic events, here the challenge comes from when we  try to isolate “events” in order to create a value of “Frequency” and standard mean and deviation.

  • One example comes from when considering heat waves. At the present time the South of Europe is suffering what it can be called a “persistent” heat wave. Since the consistency of this event is getting prolonged in time, it might be considered as just one event over 14 days. However, if in a different year you have high temperatures in periods of 3 days separated by just one day, we could count 3 heat waves. And we can have a different interpretation over what they represent. A single scenario for which its reality is becoming increasingly feasible under the present circumstances, or isolated events to be counted separately?

Heat Waves Spain by Diego Fdez-SevillaHeat waves have the particularity of behaving as drops of a fluid or waves at the coast. They can behave independently, or they can coalescence and become a tide of heat. And that is what it looks like it is happening in the South of Europe (e.g. Spain).

1st week monthly intervals Temp Anomaly Wester Europe 2015 by Diego Fdez-Sevilla Conclusions

Weather is considered as a contained event in time and location. It seems to me that Climate is being treated like trying to know when somebody is an adult, not based on attitude, but age.

If based on natural variability it is required that our environment has to have changed already in order for us to identify that it is changing, I see a limitation in the methodology which can originate many problems in the near future.

I believe that instrumental methodologies as well as biological indicators all over the world, inland and at the Oceans, are showing many symptoms of a change going on. And, as we have seen at the beginning of this post, what happens at the surface of our planet is contributing to this change.

Global picture of land surface temperature anomalies for June 30 to July 9.

Here one example of looking at bio-indicators:

“Climate change impacts on bumblebees converge across continents.” Science 10 July 2015. Kerr et al.

Responses to climate change have been observed across many species. There is a general trend for species to shift their ranges poleward or up in elevation. Not all species, however, can make such shifts, and these species might experience more rapid declines. Kerr et al. looked at data on bumblebees across North America and Europe over the past 110 years. Bumblebees have not shifted northward and are experiencing shrinking distributions in the southern ends of their range. Such failures to shift may be because of their origins in a cooler climate, and suggest an elevated susceptibility to rapid climate change.

Abstract: For many species, geographical ranges are expanding toward the poles in response to climate change, while remaining stable along range edges nearest the equator. Using long-term observations across Europe and North America over 110 years, we tested for climate change–related range shifts in bumblebee species across the full extents of their latitudinal and thermal limits and movements along elevation gradients. We found cross-continentally consistent trends in failures to track warming through time at species’ northern range limits, range losses from southern range limits, and shifts to higher elevations among southern species. These effects are independent of changing land uses or pesticide applications and underscore the need to test for climate impacts at both leading and trailing latitudinal and thermal limits for species.

 —- xxx —-

(This post is part of a more complex piece of independent research. I don´t have founding, political agenda or publishing revenues from visits. Any scientist working in disciplines related with the topics that I treat in my blog knows how to judge the contribution that my work could potentially add to the state of knowledge. Since I am in transition looking for a position in research, if you are one of those scientists, by just acknowledging any value you might see from my contribution, would not only make justice to my effort as independent researcher, but ultimately, it will help me to enhance my chances to find a position with resources to further develop my work.

I believe that the hypothesis that I have presented in previous posts in this blog (here,here and here) could help to understand present and possible future scenarios in atmospheric circulation. However, this is an assessment based on observation which needs to be validated throughout open discussion and data gathering. So please feel free to incorporate your thoughts and comments in a constructive manner.

If you feel like sharing this post I would appreciate to have a reference about the place or platform, by private or public message, in order for me to have the opportunity to join the debate and be aware of the repercussion which might generate d.fdezsevilla(at)

For anybody interested in the posts related with this discussion here I leave you those more relevant in chronological order (there are comments bellow some of them. Please check them out):

About Diego Fdez-Sevilla, PhD.

Data policy The products processed by "Diego Fdez-Sevilla PhD" are made available to the public for educational and/or scientific purposes, without any fee on the condition that you credit "Diego Fdez-Sevilla PhD" as the source. Copyright notice: © Diego Fdez-Sevilla PhD 2013-2019 orcid: and the link to its source at diegofdezsevilla.wordpress or permanent DOI found at Reearchgate. Should you write any scientific publication on the results of research activities that use Diego Fdez-Sevilla PhD products as input, you shall acknowledge the Diego Fdez-Sevilla's PhD Project in the text of the publication and provide an electronic copy of the publication ( If you wish to use the Diego Fdez-Sevilla PhD products in advertising or in any commercial promotion, you shall acknowledge the Diego Fdez-Sevilla PhD Project and you must submit the layout to Diego Fdez-Sevilla PhD for approval beforehand ( The work here presented has no economic or institutional support. Please consider to make a donation to support the means for making sustainable the energy, time and resources required. Also any sponsorship or mentoring interested would be welcome. Intellectual Property This article is licensed under a Creative Commons Attribution 4.0 International License. By Diego Fdez-Sevilla, PhD. More guidance on citing this web as a source can be found at NASA webpage:! For those publications missing at the ResearchGate profile vinculated with this project DOIs can be generated on demand by request at email: d.fdezsevilla(at) **Author´s profile: Born in 1974. Bachelor in General Biology, Masters degree "Licenciado" in Environmental Sciences (2001, Spain). PhD in Aerobiology (2007, UK). Lived, acquired training and worked in Spain, UK, Germany and Poland. I have shared the outcome from my work previous to 2013 as scientific speaker in events held in those countries as well as in Switzerland and Finland. After 12 years performing research and working in institutions linked with environmental research and management, in 2013 I found myself in a period of transition searching for a new position or funding to support my own line of research. In the current competitive scenario, in order to demonstrate my capacities instead of just moving my cv waiting for my next opportunity to arrive, I decided to invest my energy and time in opening my own line of research sharing it in this blog. In March 2017 the budget reserved for this project has ended and its weekly basis time frame discontinued until new forms of economic and/or institutional support are incorporated into the project. The value of the data and the original nature of the research presented in this platform and at LinkedIn has proved to be worthy of consideration by the scientific community as well as for publication in scientific journals. However, without a position as member of an institution, it becomes very challenging to be published. I hope that this handicap do not overshadow the value of my achievements and that the Intellectual Property Rights generated with the license of attribution attached are respected and considered by the scientist involved in similar lines of research. **Any comment and feedback aimed to be constructive is welcome as well as any approach exploring professional opportunities.** In this blog I publish pieces of research focused on addressing relevant environmental questions. Furthermore, I try to break the barrier that academic publications very often offer isolating scientific findings from the general public. In that way I address those topics which I am familiar with, thanks to my training in environmental research, making them available throughout my posts. (see "Framework and Timeline" for a complete index). At this moment, 2019, I am living in Spain with no affiliation attachments. Free to relocate geographically worldwide. If you feel that I could be a contribution to your institution, team and projects, don´t hesitate in contact me at d.fdezsevilla (at) or consult my profile at LinkedIn, ResearchGate and Also, I'd appreciate information about any opportunity that you might know and believe it could match with my aptitudes. The conclusions and ideas expressed in each post as part of my own creativity are part of my Intellectual Portfolio and are protected by Intellectual Property Laws. Licensed under Creative Commons Attribution-NonCommercial conditions. In citing my work from this website, be sure to include the date of access and DOIs found at the Framework and Timeline page and ResearchGate. (c)Diego Fdez-Sevilla, PhD, 2018. Filling in or/and Finding Out the gaps around. Publication accessed 20YY-MM-DD at ***
This entry was posted in Aerobiology, Aerosols, Energy Balance, Environmental Resilience, Extreme climatic events, Filling in, Polar vortex and Jet Stream and tagged , , , , . Bookmark the permalink.

3 Responses to Atmospheric Dynamics Absorbing Ground Emissions. Wildfires On The Ground and Smoke Up In The Sky (by Diego Fdez-Sevilla PhD)

  1. Pingback: Something for the curious minds. Climate and Streamlines (by Diego Fdez-Sevilla) | diego fdez-sevilla

  2. Pingback: Climate and weather December 2015. Another Polar Vortex another Heat Wave? (by Diego Fdez-Sevilla) | diego fdez-sevilla

  3. Pingback: Atmospheric Circulation and the Mixing Zone. (by Diego Fdez-Sevilla) | diego fdez-sevilla

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