Sentences with phrase «oceanic effects on»

Climate is simply a product of the current balance in the troposphere between the solar and oceanic effects on the positions and intensities of all the global air circulation systems

The rest of the debate is just fluff.but interesting nonetheless because the implications of that conclusion as regards climate are very profound.and lead back to my stuff elsewhere about the top down solar effects and bottom up oceanic effects on the surface pressure distribution and the shifting to and fro of the climate zones.

24) Climate in any given location is simply a product of the current balance in the troposphere between the solar and oceanic effects on the positions and intensities of all the global air circulation systems

The irregularity of the temperature changes within those main background trends can not have been anything to do with humanity and can adequately be catered for by varying oceanic effects on multidecadal time scales.

Not exact matches

As a junior studying geography at Colgate University, Jake extensively researched the negative effects of single - use plastic on the oceanic ecosystem for his final thesis.

In July, the Office of Naval Research made a survey in the waters off Virginia Beach, Virginia using ScanEagle UAVs to study the effect of oceanic and atmospheric changes on radar and radio waves, with the aim of improving military communications and the ability of radar to detect hostile craft..

The group exhibition «Tidalectics» presents 13 artists whose distinctive works cast oceanic perspectives on the cultural, political and biological dimensions of the oceans, examining the effects of human - made issues, such as climate change and sea - level rise, while reimagining human and «more - than - human» relationships.

Azumi Kuroyanagi, Régine E. da Rocha, Jelle Bijma, Howard J. Spero, Ann D. Russell, Stephen M. Eggins, Hodaka Kawahata, Effect of dissolved oxygen concentration on planktonic foraminifera through laboratory culture experiments and implications for oceanic anoxic events, Marine Micropaleontology, Volume 101, May 2013, Pages 28 - 32, ISSN 0377 - 8398, http://dx.doi.org/10.1016/j.marmicro.2013.04.005.

If so, I think we want to include tightly coupled chemical and biological processes, in that case — for example, the chemical fate of atmospheric methane over time, the effects of increasing atmospheric CO2 on oceanic acid - base chemistry, and the response of the biological components of the carbon cycle to increased temperatures and a changing hydrologic cycle.

This study, published in the February 22, 2007 edition of the review Nature, should allow us to better understand and therefore better predict the effects of climate change on oceanic circulation.

In shallower waters, it's undeniable that increased CO 2 levels result in a decreased oceanic pH, which has a profound negative effect on corals.

The mechanism by which the effect of oceanic variability over time is transferred to the atmosphere involves evaporation, conduction, convection, clouds and rainfall the significance of which has to date been almost entirely ignored due to the absence of the necessary data especially as regards the effect of cloudiness changes on global albedo and thus the amount of solar energy able to enter the oceans.

There is absolutely no reason to believe that this effect will do anything but get stronger from here on as the vast «crops» of oceanic bacteria adapt to both warmer ocean waters and increased CO2 and nutrient levels and simply increasingly cool the global atmospheric climate simply by «growing faster»!

«The atmospheric greenhouse effect is a flea on the back of an oceanic elephant and the influence of CO2 but a microbe on the back of the flea and the influence of anthropogenic CO2 but a molecule on the back of the microbe.»

It logically follows that, from time to time, the other oceanic cycles can operate in conjunction with PDO / ENSO to emphasise the effect on the global temperature.

The moon raises oceanic and solid Earth tides which by a secondary effect it exerts a gravitational drag on the Earth's rotation.

Requires the Climate Service Program to: (1) analyze the effects of weather and climate on communities; (2) carry out observations, data collection, and monitoring of atmospheric and oceanic conditions; (3) provide information and technical support to governmental efforts to assess and respond to climate variability and change; (4) develop systems for the management and dissemination of data; (5) conduct research to improve forecasting and understanding of weather and climate variability and change and its effects on communities; and (6) develop tools to facilitate the use of climate information by local and regional stakeholders.

However all other effects on global albedo are trivial as compared to the effects of solar and oceanic forcing.

Once the sign of the solar effect on the stratosphere is reversed it becomes possible to propose a system of climate change arising simply from the latitudinal shifting of the air circulation systems in response to competing forces from variable oceanic and solar cycles.

There are also a number of effects which can have a large impact on short - term temperatures, such as oceanic cycles like the El Niño Southern Oscillation or the 11 - year solar cycle.

What additional research do you think would need to be done to fully explore the effects of ocean acidification on the oceanic biological pump?

Remember that there is a variable lag between the initial solar effect of warming or cooling on the Pacific Ocean and that effect then working through all the other oceanic oscillations so it is difficult to establish the overall balance of the oceanic oscillations at any given time.

The climatic system / oceanic system are driven by the sun, therefore it stands to reason any changes in solar output (variations) will have an effect on these two systems which in turn will have an effect on the climate.

The effects on biodiversity are likely to be much less severe in the open ocean than in estuaries and wetlands, where species in shallow, restricted impoundments would be affected long before deep - oceanic species.

Until climatologists can properly make models that reflect the entire global history and take into account plate position and how high the plates ride, oceanic levels due to this and the position of oceans, overall insolation, overall daylength and its effects on average global temperature and factor in known carbon dioxide levels over that time period, then they will be unable to give any correlation between current carbon dioxide levels and global temperature.

http://illconsidered.blogspot.com/2006/04/historically-co2-never-causes.html 100 years of shift does not factor into the larger scale phenomena http://illconsidered.blogspot.com/2006/01/one-hundred-years-is-not-enough.html Until climatologists can properly make models that reflect the entire global history and take into account plate position and how high the plates ride, oceanic levels due to this and the position of oceans, overall insolation, overall daylength and its effects on average global temperature and factor in known carbon dioxide levels over that time period, then they will be unable to give any correlation between current carbon dioxide levels and global temperature.

I think this is a critical issue for the entire AGW construct because if the extra DLR from more GHGs can not add to ocean heat content then only the effects on the air need be considered and that would be insignificant in the face of oceanic control of surface air temperatures.

As you may recall I say that the ocean phases also have an effect so if you have a weak ocean phase when there are a lot of sunspots the lack of poleward pressure from the weak oceanic influence fails to take full advantage and allows the AO to remain stronger than it otherwise would be on the basis of solar activity levels alone.

The oceanic effect is always dominant but the fact is that on 500 year timescales (not necessarily on shorter time scales due to interference from lesser cycles and chaotic variability) the sun is less active as per the Maunder Minimum and at the same the oceans were independently releasing energy at a low rate.

«On the basis of the information in the public domain about solar cycles and the positive PDO it should have been blatantly obvious that the world would warm up without the need to speculate on a contribution from CO2 or anything else... I find Mr. [Alec] Rawls very helpful in illustrating the effect of time lags between solar input and oceanic oscillations... As Mr. Rawls points out.On the basis of the information in the public domain about solar cycles and the positive PDO it should have been blatantly obvious that the world would warm up without the need to speculate on a contribution from CO2 or anything else... I find Mr. [Alec] Rawls very helpful in illustrating the effect of time lags between solar input and oceanic oscillations... As Mr. Rawls points out.on a contribution from CO2 or anything else... I find Mr. [Alec] Rawls very helpful in illustrating the effect of time lags between solar input and oceanic oscillations... As Mr. Rawls points out...

Any variability in oceanic circulation could have strong effects on local, and hence average temperature, even with a fixed energy budget.

The presence of the longer - term effects on Australian rainfall from oceanic shifts, such as the Pacific Decadal Oscillation (PDO) and Interdecadal Pacific Oscillation (IPO), make the analysis of this situation, and the teasing out of the AGW influence, a complex matter.

One hypothesis why CO2 has no significant effect on temperatures is that much of the Earth, particularly in the tropical oceanic areas which receive much of the energy from the sun are regulated by emerging climate phenomena, not CO2, and these are what primarily determine temperatures in these areas.

Predictions concerning the consequences of the oceanic uptake of increasing atmospheric carbon dioxide (CO2) have been primarily occupied with the effects of ocean acidification on calcifying organisms, particularly those critical to the formation of habitats (e.g. coral reefs) or their maintenance (e.g. grazing echinoderms).

1) Abstract «Such changes could have significant ramifications for global sea level, the ocean thermohaline circulation, native coastal communities, and commercial activities, as well as effects on the global surface energy and moisture budgets, atmospheric and oceanic circulations, and geosphere - biosphere feedbacks.

The latter, which isolated Antarctica within a cold polar sea, produced global effects on atmospheric and oceanic circulation.

Topics that I work on or plan to work in the future include studies of: + missing aerosol species and sources, such as the primary oceanic aerosols and their importance on the remote marine atmosphere, the in - cloud and aerosol water aqueous formation of organic aerosols that can lead to brown carbon formation, the primary terrestrial biological particles, and the organic nitrogen + missing aerosol parameterizations, such as the effect of aerosol mixing on cloud condensation nuclei and aerosol absorption, the semi-volatility of primary organic aerosols, the importance of in - canopy processes on natural terrestrial aerosol and aerosol precursor sources, and the mineral dust iron solubility and bioavailability + the change of aerosol burden and its spatiotemporal distribution, especially with regard to its role and importance on gas - phase chemistry via photolysis rates changes and heterogeneous reactions in the atmosphere, as well as their effect on key gas - phase species like ozone + the physical and optical properties of aerosols, which affect aerosol transport, lifetime, and light scattering and absorption, with the latter being very sensitive to the vertical distribution of absorbing aerosols + aerosol - cloud interactions, which include cloud activation, the aerosol indirect effect and the impact of clouds on aerosol removal + changes on climate and feedbacks related with all these topics In order to understand the climate system as a whole, improve the aerosol representation in the GISS ModelE2 and contribute to future IPCC climate change assessments and CMIP activities, I am also interested in understanding the importance of natural and anthropogenic aerosol changes in the atmosphere on the terrestrial biosphere, the ocean and climate.

Northward atmospheric winter fluxes are observed after the enhanced global warming after 1970, and, for the first time over the period considered, a positive correlation is observed between atmospheric and oceanic reducing effects on the ice extent.