Sentences with phrase «heat balance over»

The only thing that has been changing in a way that should increase global heat balance over the last 40 years are greenhouse gases.

«On the Observed Annual Cycle in the Ocean - Atmosphere Heat Balance over the Northern Hemisphere.»

The increase in ocean heat content is much larger than any other store of energy in the Earth's heat balance over the two periods 1961 to 2003 and 1993 to 2003, and accounts for more than 90 % of the possible increase in heat content of the Earth system during these periods.

Not exact matches

Balance of payment deficits of an unprecedented magnitude have resulted in credit induced economic over heating on a global scale.

I tweaked the seasonings for over two years until I came up with, what I think is, the perfect balance of smokiness and heat.

Heat a large sauté pan over medium - high heat and add extra virgin olive oil or Earth Balance butHeat a large sauté pan over medium - high heat and add extra virgin olive oil or Earth Balance butheat and add extra virgin olive oil or Earth Balance butter.

Add your butter or Earth Balance to a large pot over medium heat.

put the sugar, earth balance, honey, and salt in a medium saucepan over medium - high heat.

put the earth balance, almond milk, and vanilla in a small saucepan over medium heat.

2 medium - large white, baking or Yukon gold potatoes, peeled (reserve skin) and cubed to make 3 cups 1 tablespoon olive oil 1 tablespoon vegan butter (I like Earth Balance) pinch of salt 1/2 teaspoon of Liquid Smoke 3/4 cup chopped onion (medium fine) 1/2 cup chopped celery (split stalks lengthwise and slice crosswise fairly thinly) 1/2 teaspoon dried thyme 1 teaspoon kelp granules (you could try powdered kelp, though I haven't tested it) salt and freshly ground black pepper to taste 3 cups vegetable broth, warmed in the microwave or in a saucepan 2 cups unsweetened soy milk, also warmed in the microwave or in a saucepan (may combine with broth to heat) 1 cup coarsely chopped homemade «seafood seitan» (see below) or Shitake or oyster mushrooms, sauteed in a skillet with 1 - 2 teaspoons olive oil for 2 - 3 minutes over medium - high heat, seasoned to taste with granulated kelp (in place of salt) liquid smoke to taste 2 tablespoons minced fresh parsley Optional garnish: a teaspoon of fresh minced parsley and a tiny pinch of Old Bay seasoning per bowl

Heat a wide nonstick skillet over medium - high heat, then add the Earth BalaHeat a wide nonstick skillet over medium - high heat, then add the Earth Balaheat, then add the Earth Balance.

Add the earth balance to a skillet over medium to medium - high heat.

heat it over medium - high heat until the earth balance is melted, then turn the heat down to low and let it simmer for 5 minutes.

Lastly, I drizzled a little honey over the pasta because I felt it needed a little sweetness to balance out the heat of the pepper.

While the skewers are cooking over the coals, you paint them with the reduced marinade to build up flavor and color, and by the end, you have a supremely juicy, beautifully - colored nuggets of dark meat with just the right about of peppery heat balanced by sweet molasses and punchy ginger.

Stole it right back, all momenutum killed for the Heat — game 4 in the balance with Jojo's shadow back in the paint looming over their greatest strenght — attacking the basket.

A group of small filter - feeding invertebrates had taken over on top of the heated panels, completely shifting the balance of the tiny test ecosystem.

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For over half a century, pet food manufacturers have claimed that because carbohydrate - based, heat processed pet foods are «nutritionally complete and balanced», they are superior to anything companion pets might otherwise consume.

Given that the cryosphere and oceans are far better long - term indicators of changes in Earth's energy balance than the much more «noisy» troposphere, for anyone to suggest that the warming of the Earth system has slowed or stopped over the past 10 years, means they are purposely ignoring the far bigger heat sinks of the cryrosphere and oceans, or they simply want to spout nonsense.

Because latent heat release in the course of precipitation must be balanced in the global mean by infrared radiative cooling of the troposphere (over time scales at which the atmosphere is approximately in equilibrium), it is sometimes argued that radiative constraints limit the rate at which precipitation can increase in response to increasing CO2.

In its simplest form averaged over a year, can not the ocean heat balance be expressed as:

The radiative balance over equilibrium timescales — the heat released by raindrop formation will locally warm the atmosphere, but it takes time for the atmospheric circulation to average this out.

If the tropopause level LW flux were ever saturated over the whole LW portion of the spectrum, and there were still significant solar heating below that level, then the tropopause would tend to shift upward to where the LW flux is not saturated at some frequencies; in an equilibrium climate, the net LW flux out of the tropopause has to balance SW heating below the tropopause (in the approximation of zero non-radiative flux out of the tropopause), and thus can not be zero.

I think a major aspect of the balance has been glossed over: the ocean is heated mainly by the visible part of the spectrum, the energetic part of the sun's glare.

Re my 441 — competing bands — To clarify, the absorption of each band adds to a warming effect of the surface + troposphere; given those temperatures, there are different equilibrium profiles of the stratosphere (and different radiative heating and cooling rates in the troposphere, etc.) for different amounts of absorption at different wavelengths; the bands with absorption «pull» on the temperature profile toward their equilibria; disequilibrium at individual bands is balanced over the whole spectrum (with zero net LW cooling, or net LW cooling that balances convective and solar heating).

As budget negotiations heat up, so does the debate over the balance between investments in the long - term future and short - term necessities.

Second, energy in vs. energy out of the system can hardly balance until we have a better handle on the circulation of the ocean (over 95 % of the heat capacity of Earth) and its rate of heat uptake.

If coffee at 70 C is poured in, the heating element will, over time, cause the coffee to hit its equilibrium temperature where the heat in from the heating element is exactly balanced by the heat lost to ambient through the thermos walls.

This was my mental equation dF = dH / dt + lambda * dT where dF is the forcing change over a given period (1955 - 2010), dH / dt is the rate of change of ocean heat content, and dT is the surface temperature change in the same period, with lambda being the equilibrium sensitivity parameter, so the last term is the Planck response to balance the forcing in the absence of ocean storage changes.

«The forcing should not balance the ocean heat content increase, and it should apply over the same period anyway (1955 - 2010) which 1.6 W / m2 doesn't.»

... and toward the end of summer, the most powerful heat engines take over to «balance» any remaining «excess» heat.

-- the overall change to the global heat balance climate from basic physics bounded by paleo observations (over time increasingly constrained by modern observations)-- the probable overall patterns of regional change at a large scale — the range of impacts.

Over land, you have a surface energy balance that includes downwelling IR, upwelling IR (Stefan Boltzmann), downwelling solar radiation minus what is reflected back from the surface, latent heat flux and sensible heat flux (these are turbulent fluxes associated with exchange with the atmosphere), and conductive flux from the ground (below the surface).

That we should not expect that heat, as such, in that location, to have any substantive effect on climate... as it corresponds to fractions of a degree over the entirety of the ocean and has no effect on the energy balance.

Drought changes the balance between latent and sensible heat over land surfaces — increasing temperature readings.

This popular balance models the earth as a ball suspended in a hot fluid with heat / energy / power entering evenly over the entire ToA spherical surface.

Over land evaporation is limited by water availability — and so the balance of latent and sensible heat changes with rain and drought.

Over the coastal escarpment, the regression coefficients of temperature anomalies with the SAM are an indication that the SAM is tied with the surface energy balance and modulation of the thermally direct circulation as described by Parish and Bromwich (2007); the katabatic winds mix sensible heat towards the surface to balance longwave cooling (van den Broeke et al. 2006).

«The assessment is supported additionally by a complementary analysis in which the parameters of an Earth System Model of Intermediate Complexity (EMIC) were constrained using observations of near - surface temperature and ocean heat content, as well as prior information on the magnitudes of forcings, and which concluded that GHGs have caused 0.6 °C to 1.1 °C (5 to 95 % uncertainty) warming since the mid-20th century (Huber and Knutti, 2011); an analysis by Wigley and Santer (2013), who used an energy balance model and RF and climate sensitivity estimates from AR4, and they concluded that there was about a 93 % chance that GHGs caused a warming greater than observed over the 1950 — 2005 period; and earlier detection and attribution studies assessed in the AR4 (Hegerl et al., 2007b).»

For the real earth, with a significant heat capacity and significant atmospheric and ocean transport, the one summary number that has meaning is the average of T ^ 4 over the surface of the earth... That is what is going to go into determination of the global surface radiative balance.

A: The volume integral (heat balance equation) as presented in Pielke (2003) http://blue.atmos.colostate.edu/publications/pdf/R-247.pdf suggests that the changes in ocean heat storage averaged over a year are a snapshot of the radiative imbalance at the top of the atmosphere.

If you have good measurements of upper ocean and atmospheric temperatures, then if you had a good decade - long satellite record of the Earth's total radiative energy balance from space — say, if Triana has been launched to in the late 1990s — then you could use conservation of energy to calculate the rate of heat uptake by the deep ocean over the past ten years.

Over the longer term the accuracy is better, there is less wiggle room, and in fact we are able to balance out the energy flows — i.e. the increase in ocean heat content is pretty much what is expected from the anticipated radiative imbalance (see the figure).

Over long time periods, this tropical heat uptake is roughly balanced by heat release from the ocean to the atmosphere in other regions closer to the poles.

Present global climate models (GCMs) supersede the old simple conceptual models on the greenhouse effect, some of which include radiative - convection and heat balance models discussed over the period 1890 — 1980 (Arrhenius 1896; Hulburt 1931; Charney et al. 1979; Schneider and Dickinson 1974; North 1975; Wang WC and Stone P 1980).

From your calculations, relate the heat balance to global climate over these 10 Ma flitches.

They then used air bubbles trapped in those ice cores to calculate the Earth's energy balance — whether the planet was adding or losing heat to space — over the period.

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