A Climate “Between Waters” (by Diego Fdez-Sevilla).


A Climate “Between Waters” (by Diego Fdez-Sevilla).

(Citation. Diego Fdez-Sevilla, A Climate “Between Waters”. http://www.diegofdezsevilla.wordpress.com and DOI: 10.13140/RG.2.1.1697.5847
2015-09-11 T 17:28:47 UTC

After a pretty warm summer, the Mediterranean sea has plenty of heat in store to supply humidity into the atmosphere and energise all the present and near future burst of cold air carried by the weak jet stream that we have.

Jet Stream over Iberian Peninsula DiegoFdezSevilla

SST Iberian Peninsula 7th Sept 2015

Spain is going through a phase of contrasts where the Atlantic side keeps dry and colder than the Mediterranean side with plenty of severe weather events causing flooding and wind related situations.

7e58fb84-5ad5-4319-99fb-022c4eab609f-original

Satellite image Europe 7th Sept 2015 DiegoFdezSevillaEurope Water vapour top of the atmosphere DiegoFdezSevilla

Floods in the Penninsula

Wind and Tornadoes in Ibiza. (Balear Islands)

Hail like golf balls breaking car windows and killing 80% Flamenco population in a nearby Laguna in Albacete.

Follow up from previous research presented in this blog.

I believe that the present weather events, altogether with the tornado seen in Venice on July, represent some of the new “Drops of Weather” coming over to say that the Summer, as we know it, is coming to an end.

The reason behind it seems to be the sporadic and unpredictable behaviour of the Jet stream, which not only is wobbly in latitude, but also in the vertical profile of the atmosphere. Accordingly, we can see that when it comes to lower levels from 300hPa induces alterations in the thermodynamical behaviour of the tropospheric circulation. In turn, when this cold air touches the lower level of our atmosphere, activates the energy accumulated in the Water vapour contained in it as latent heat, delivering new forms of energy; kinetic provoking strong winds, electrostatic generating lightnings and potential carried in the mass of all the water coming from its gaseous state into liquid or solid precipitation.

I have already discussed what is my theory about what it is happening that it is generating such a wobbly jet stream in latitude and altitude. This theory was published in a previous post and it points out the incorporation of masses of water vapour into polar latitudes as consequence of CO2 forcing as the cause wearing out the strength of the Polar Jet Stream.

I also have suggested that such incorporation of masses of water vapour into Polar Latitudes follow channels which are linked with persistent cyclonic events in the Atlantic and the Pacific. The present patterns seen in the circulation over the Pacific and the Atlantic are consistent with those proposed in this theory.

We can compare present circulation:

7th Sept 2015 TPW Atlantic DiegoFdezSevilla

Water vapour circulation globally 7th Sept 2015 DiegoFdezSevilla

Patterns proposed in the theory:

Surface Wind TPW DiegoFdezSevilla

Ultimately, if this theory is right and weather patterns are incorporating water vapour into Polar latitudes, it would affect:

  • The strength of the Polar Jet Stream becoming wobbly from the bottom up, from tropospheric circulation forcing instead of from the stratospheric Polar vortex, (more here)
  • Introduction of water vapour into Arctic Polar latitudes would decrease temperature gradients in the Pole reducing ice and snow cover, (more here)
  • that would induce ice melting which in turn would affect SST and Oceanic circulation in the Atlantic and Pacific. That would explain the cold anomaly in SST in the North Atlantic, thus the AMOC and global thermohialine circulation going around the Antarctic and arriving at the Pacific.(more here)
  • Arctic Polar masses of air getting warmed up would become involved in translatitudinal circulation from the Atlantic and the Pacific through the Arctic, in a breathing like cycle. That would open a new channel for balancing gradients of atmospheric pressure between the atmospheric masses of air above both Oceans. That would explain the synchronicity between Low pressures observed in the North Atlantic and North Pacific,(more here)
Arctic Dynamics Breathing IN-OUT by Diego Fdez-Sevilla

Atmospheric Dynamics in the Arctic. Breathing IN&OUT. Total Precipitable Water circulation patterns over the North Atlantic and North Pacific Oceans on the 13th June 2015 and 7th Sept 2015. Images generated by Nullschool.net from NOAA NCEP/GFS. The days chosen for this images have been selected to represent the conditions mentioned. The periodicity of the two scenarios is variable and it is not represented by the lap of time between the dates. This work is registered and protected by authorship laws.

Arctic Dynamics IN-OUT Diego Fdez-Sevilla

Atmospheric Dynamics in the Arctic. Breathing IN&OUT. Water Vapour circulation patterns over the North Atlantic and North Pacific Oceans on the 29th August 2015 and 7th Sept 2015. Images generated by Satellite GOES8 WV. The days chosen for this images have been selected to represent the conditions mentioned. The periodicity of the two scenarios is variable and it is not represented by the lap of time between the dates. This work is registered and protected by authorship laws.

  • An interconnection between Atlantic and Pacific atmospheric circulation through the Arctic would affect Equatorial winds. That would have an impact over the distribution of SST being dominated by them, being the most relevant the ENSO.(more here and here)
  • Furthermore,  new channels breaking the restriction of keeping warm masses of air bellow Polar circulation would release the thermodynamical limits for equatorial latitudes to absorb water and heat, therefore, increasing thermal conductivity towards upper latitudes. That would explain heat waves moving upward in latitude.(more here and here)
  • At the same time, incorporating the possibility for subtropical circulation to occupy the volume of space at Polar latitudes would allow the global circulation to absorb more energy without steep increases in temperature thanks to the extra volume added to be occupied.(more here)
  • An homogenization in the amount of energy carried in the atmosphere by water vapour would induce a decrease between gradients of energy. That would allow atmospheric events to persist in location and time due to the reduced capacity of the atmosphere to dissipate its energy.(more here)
  • The amount of energy being accommodated by the atmosphere would behave like electricity, being tamed by the capacity of the surroundings to absorb and conduct it. But, like a short circuit, the energy contained in the atmosphere, could overwhelm the capacity for the surroundings to cope with it in a smoothly manner, triggering abrupt discharges from energy in latent heat form carried by the water vapour, into potential energy carried by the masses of water in form of hail and  rain, and kinetic energy generating strong winds. All those forms of energy capable of decimating crops, houses and even killing animals as we have seen in some videos in this post.(more here)

Most definitely, I believe that the climate in our Earth is what it lies between waters. Between cold waters and warms waters, between waters in the atmosphere or those in the ground inland or at the oceans. Altogether, our climate lies on those processes moving energy between waters in the form of gas, liquid or solid.

Any comments or thoughts are welcomed. I would please ask for any indication if any discussion or debate incorporates my thoughts so I can join in.

—- 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)gmail.com)

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):

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About Diego Fdez-Sevilla, PhD.

Citing This Site "Title", published online "Month"+"Year", retrieved on "Month""Day", "Year" from http://www.diegofdezsevilla.wordpress.com. By Diego Fdez-Sevilla, PhD. More guidance on citing this web as a source can be found at NASA webpage: http://solarsystem.nasa.gov/bibliography/citations#! 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 previous work as scientific speaker in events held in those countries as well as in Switzerland and Finland. After couple of years performing research and working in institutions linked with environmental research and management, I find myself in a period of transition searching for a new position or funding to support my research. In the present competitive scenario, instead of just moving my cv and wait for my next opportunity to arrive, I have decided to invest also my energy and time in opening my own line of research showing what I am capable of. The value of the data and the original nature of the research presented in this blog 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 work and the intellectual rights represented by the license of attribution attached are respected and considered by the scientist involved in this line of research. Any comment and feedback aimed to be constructive is welcome. 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, 2017, 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) gmail.com or consult my profile at LinkedIn, ResearchGate and Academia.edu. 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. (c)Diego Fdez-Sevilla, PhD, 2016. Filling in or Finding Out the gaps around. Publication accessed 20YY-MM-DD at http://www.diegofdezsevilla.wordpress.com/
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77 Responses to A Climate “Between Waters” (by Diego Fdez-Sevilla).

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