Sentences with phrase «cool ocean influenced»

True Myth wines embrace the best of San Luis Obispo County — Chardonnay from the cool ocean influenced Edna Valley and Cabernet from the rugged terrain of Paso Robles.

Not exact matches

Science questions the answers, e.g. hurricanes are caused by warm moist ocean air being drawn up into the cooler atmosphere and creating a wind pattern though we are still open to consider other factors that may have influence on this cycle.

The entire region is above 1000 feet elevation and receives cooling Pacific Ocean influences.

He points to the influence of the Pacific Ocean, which can make winters warm in California and summers cool.

That region, he says, is susceptible to even small amounts of warming and cooling from the atmosphere — and how cold the water gets influences how much or how little it sinks, thereby driving or delaying, respectively, the ocean conveyer belt.

Covering nearly 5.5 million square miles, the frozen mass exerts an enormous influence on the global climate, reflecting sunlight back into space and cooling Earth's atmosphere and oceans.

It is also not influencing increased ocean heat content, melting ice caps and glaciers, satellites showing tropospheric warming or strato cooling, etc

While not nearly as dramatic, the influence of solar, ocean, and wind patterns is much more immediate, but these effects generally alternate between warming and cooling over the course of months to decades in relation to their respective cycles.

ENSO events, for example, can warm or cool ocean surface temperatures through exchange of heat between the surface and the reservoir stored beneath the oceanic mixed layer, and by changing the distribution and extent of cloud cover (which influences the radiative balance in the lower atmosphere).

Enjoy a flight of Migration wines in this stunning location tempered by cool marine influence from the Pacific Ocean.

This is due to the influence of the cool California Current that sweeps through this division of the Pacific Ocean.

ENSO events, for example, can warm or cool ocean surface temperatures through exchange of heat between the surface and the reservoir stored beneath the oceanic mixed layer, and by changing the distribution and extent of cloud cover (which influences the radiative balance in the lower atmosphere).

What happens to global temperature trends when you factor in the potentially confounding influence of ocean warming and cooling cycles?

As you may be aware, those rejecting the enormous body of evidence pointing to a growing human influence on climate had embraced some transitory findings implying that the oceans were cooling.

It's important to note that a substantial short - term influence on the globe's average temperature, the cycle of El Niño warmth and La Niña cooling in the tropical Pacific Ocean, was in the warm phase until May but a La Niña cooling is forecast later this year, according to the Climate Prediction Center of the National Oceanic and Atmospheric Administration.

While the aerosol influence last less than a decade, the influence on surface temperatures continues because of the slow mixing of cooled waters on the ocean surface.

as we can we may be able to influence albedo on an ocean scale — and hopefully create a little bit of global cooling.

The global temperature switches from cooling to warming mode frequently as a result of the ever changing interplay between variations in solar influence and intermittent heat flows from the oceans.

The aim of the C - SIDE working group is to reconstruct changes in sea - ice extent in the Southern Ocean for the past 130,000 years, reconstruct how sea - ice cover responded to global cooling as the Earth entered a glacial cycle, and to better understand how sea - ice cover may have influenced nutrient cycling, ocean productivity, air - sea gas exchange, and circulation dynaOcean for the past 130,000 years, reconstruct how sea - ice cover responded to global cooling as the Earth entered a glacial cycle, and to better understand how sea - ice cover may have influenced nutrient cycling, ocean productivity, air - sea gas exchange, and circulation dynaocean productivity, air - sea gas exchange, and circulation dynamics.

This would be some combination of warmings and coolings due to natural and / or human influences such as aerosols, instabilities in ocean currents, Length - Of - Day (LOD) fluctuations, the stadium wave (Wyatt and Curry), the 3M effect (me, December 17, Global Environmental Change section, this AGU Fall Meeting), etc. etc..

Christy is correct to note that the model average warming trend (0.23 °C / decade for 1978 - 2011) is a bit higher than observations (0.17 °C / decade over the same timeframe), but that is because over the past decade virtually every natural influence on global temperatures has acted in the cooling direction (i.e. an extended solar minimum, rising aerosols emissions, and increased heat storage in the deep oceans).

They can't get their story right — it is cooling but it's La Niña and decreasing solar intensity — or it is warming in the deep oceans but God only knows why because there are all these cooling influences.

Regardless of near term outcomes — it is odds on for a cooler sun and more upwelling in the Pacific Ocean this century — providing a cooling influence on the oceans and atmosphere and the inevitable regional variability in rainfall.

That suggests that cooling may start with changes in the ocean circulation, influencing the northern sea surface and atmosphere, said co-author Jerry McManus, a professor at Lamont - Doherty Earth Observatory.

This «hiatus» is probably due to the cooling influences from natural radiative forcings (more volcanic eruptions and reducing output from the sun as part of the natural 11 - year solar cycle) and internal variability (fluctuations within the oceans unrelated to forcings).

The existence of that cooler layer is evidence that the rate of evaporation is the primary influence on variability in the rate of ocean energy loss (apart from internal ocean circulation variability which is not relevant here) and it follows that more evaporation for the same rate of conduction and radiation (from a stable temperature differential) will send that cooler layer deeper and / or intensify the temperature differential between it and the ocean bulk below.

Preliminary comparison of solar results with observations indicates that, if the solar influence exists, it is not being manifested in terms of simple cooling; changes in the ocean - atmosphere system may be significantly modifying the response.

Atmospheric temperature at the ocean surface influences the rate at which the ocean cools.

Lansner and Pepke Pedersen (2018) point out that, due to the divergent rates of warming and cooling for land vs. ocean water, there is a significant difference in the range of temperature for the regions of the world influenced by their close proximity to oceans and coastal wind currents (ocean air affected, or OAA) and the inland regions of the world that are unaffected by ocean air effects and coastal wind because they are sheltered by hills and mountains or located in valleys (ocean air sheltered, or OAS).

I think it is time for a general update due to subsequent developments (especially the current 2 year global cooling trend and a quieter sun with cooling oceans after an 8 year temperature plateau which tends to show that my point about solar and oceanic influences on global temperatures has some merit) and the fact that I can make the essential points more simply by condensing them into a series of bullet points as follows:

The ocean cools as the atmosphere responds with characteristic El Niño weather patterns forced from the region that influence weather patterns world wide.

«A general update due to subsequent developments (especially the current 2 year global cooling trend and a quieter sun with cooling oceans after an 8 year temperature plateau which tends to show that my point about solar and oceanic influences on global temperatures has some merit)» - Stephen Wild...