Sentences with phrase «where sst»

Tropical convergence zones are also prime examples of persistently cloudy regions where SST detection by AVHRR is problematic.

vi) But at the bottom of that cascade where SST (skin) has it's interface with the subskin there is still going to be that deficit.

Figures 2b and 3b shows the region where SST is restored; within the inner box the ocean surface heat flux is fully overridden, while in the buffer zone between the inner and outer boxes, the flux is blended with the model - diagnosed one.»

If you download 1998 - 2009 cloud cover here, and sea surface temperatures here, you can see that, except for a cloud band from ~ 0 to 10 degrees N, cloudiness is generally less where SST is warmer, though there are lots of details and spatial variation that lessen the correlation.

For example, clade D Symbiodinium are more abundant in acroporid corals from back - reef lagoons in American Samoa, where the SSTs reach higher maximum temperatures than the fore - reef environments, where Acropora primarily hosts clade C. ref Because they are often found in increased abundance on reefs that are exposed to environmental stressors, the presence of clade D symbionts can be a biological indicator of negative changes in coral health.

In some cases, the perturbation integrations were initialised using data from control integrations where the SSTs were near present - day values and not pre-industrial.

Even in cases where it is cold or where SSTs [sea surface temperatures] are cold, or where water vapor is low, they are still warmer / moister than they would have been without the global warming.

The warm air rises over the Pacific Warm Pool, causing an inflow of air from the east where SSTs are cooler.

Hurricanes and typhoons currently form from pre-existing disturbances only where SSTs exceed about 26 °C and, as SSTs have increased, it thereby potentially expands the areas over which such storms can form.

Not exact matches

The regions where droughts have occurred seem to be determined largely by changes in SSTs, especially in the tropics, through associated changes in the atmospheric circulation and precipitation.

Then, we generated proxies with this fitted model, using as predictors the SST time series where the components linearly related to the MEI, PDO and AMO were removed (by linear regression, as above).

You're right 2.2 K (grid points where there is paleo - data) refers to the SST change over the ocean and SAT over land, and 3 K refers to the global SAT change.

Collaboration continues in the SST meeting, where the focus is on data assessment and problem solving.

The reason for this discrepancy seems to be that you will only get those EPA numbers if you leave the SST in Normal mode, where it gets minimal use of the turbo.

Twin Clutch SST allows the driver to choose between Autoshift fully automatic shifting and Manual Shift, where the driver can change gears as with a manual transmission.

The western pole tends to be anomalously colder than the eastern pole from 1880 to 1919, whereas in the interval 1950 — 2004 the SST anomalies over the western pole are comparable to those over the eastern pole though there are occasional outliers where the eastern pole is anomalously colder than the western pole.

What this argument fails to consider is that the greater SST also produces a more vigorous updraft, so that the rising moist air has less time in which the collision / coalescence process can work before the air reaches the upper cloud layers where spontaneous ice nucleation takes place (at somewhere around -40 C, reached near the top of the troposphere).

And it continues to this date where warmer sst's seem to spread southwards from North of the equator.

In a region where the ocean was already being heated, the same pattern would be seen but now since the skin SST was warmer, the skin - bulk difference would increase, causing more heat to go into the ocean.

Where is the mechanistic analysis that says that it is the sea ice over the last couple of years (and not SST, or north - south gradients, or strat - trop connections or whatever) that has caused this?

The wind speed is given by v ^ 2 = E (Ts - To) / To, where v is peak wind velocity, Ts is SST, To is TOA temperature, and E is a constant.

The warmpth in the southern USA and elsewhere north of the hurricane - producing region has been as large a factor in the large number of storms this season as the actual SST where the storms are formed, because it has decreased wind shear.

So, where does the 15 - year SST forecast come from, if not an ocean model?

Sorry, I was comparing heat content (not SST, neither SAT) of different parts of the oceans down to 300 m depth (where most of the variation is visible), based on the data of Levitus e.a. which can be downloaded from the NOAA web site.

Consenquently, the associated SST pattern is slightly cooler in the deep convection upwelling regions of the Equitorial Pacific and the Indian Ocean, strongly cooler in the nearest deep convection source region of the South Atlantic near Africa and the Equator, warm over the bulk of the North Atlantic, strongly warmer where the gulf stream loses the largest portion of its heat near 50N 25W, and strongly cooler near 45N 45W, which turns out to be a back - eddy of the Gulf Stream with increased transport of cold water from the north whenever the Gulf Stream is running quickly.

Of interest are pages 62 and 63, where cloud cover changes roughly coincidence with SST changes.

This view is echoed by Kerry Emanuel in comments on the paper in the Washington Post, where he suggests that the impact of wind shear changes relative to warming SSTs in the real world, as diagnosed from trends observed thus far, may be overstated by the V+S study:

I wonder if the fact the higher SSTs will lead to somewhat longer seasons (and 2005 certainly had that), and larger sea - surface area where TCs might form, would serve to counteract the effect you describe, and still lead, net - net, to an increase in the number of tropical cyclones with higher SSTs.

I compared the ENSO and volcano - adjusted data to the SST anomalies of two parts of the western Pacific (the Kuroshio - Oyashio Extension and the SPCZ Extension) where the secondary effects of ENSO appear strongest.

In 2014 there were a lot of months were SST were the warmest ever; there were several months where land was way back in the pack.

MKL present a flawed SST — intensity regression analysis comparing correlations of real - world intensities versus SST with idealized model correlations where no synoptic weather variability is present.

The PDO can not be used to estimate the contributions that the THC / MOC - induced swings in North Pacific SST have on Northern Hemisphere and global temperatures, where a residual index similar to the AMO could.

The high SSTs provide ample moisture to the atmosphere and the resulting evaporative cooling of the ocean dropped the subsequent SST values down, but meanwhile heavy rains, often record breaking in intensity, occurred nearby to where the winds carried the moisture.

Small - scale mesocosm experiments, where field populations of marine Crenarcheaota are adapted to different temperatures, will be used to further calibrate the TEX86 - SST relationship.

In an ideal world where we need accurate SST», s what would be your minimum sampling requirements in order to end up with an accurate measurement for each year in each sst grSST», s what would be your minimum sampling requirements in order to end up with an accurate measurement for each year in each sst grsst grid?

This was a fore - runner to the exceptionally heavy rains in Queensland in December 2010, and January 2011 where the southern monsoon rains kicked in with the presence of record high SSTs.

The moisture in the atmosphere, which has been widely observed to be increasing in association with increased SSTs, then gets carried around by atmospheric winds to where storms are favored.

Only looking at the Niño 3.4 index hides the fact that this event is more typical of La Niña Modoki, where cool SST anomalies in the central equatorial Pacific are flanked by warm anomalies to the east and west.

But after it initially formed near the Bahamas and drifted eastward, it was in a region where sea - surface temperatures (SSTs) are running about 3 °F above the long - term average consistent with a warmer world.

Where there is abrupt climate change in rainfall, temperature or SST for instance as we find everywhere then it simply looks like a chaotic oscillator.

Where did I write that, outside of the tropical Pacific, a rise in SST anomalies associated with an El nino event was caused by with an increase in evaporation?

Tivy (University of Alaska Fairbanks); 5.7 Million Square Kilometers; Statistical This method is based on a simple regression where the predictor is the previous summer (May / June / July) sea surface temperature (SST) in the North Atlantic and North Pacific oceans near the marginal ice zone.

The SST data where available is used up to 100 km from any coast, but data from any source is extended to a maximum radius of 1200 km if no other measured data points are present within this range.

Note where he shifts «SSTs» to «global surface temperatures?»

The data presented in this post are from the KNMI Climate Explorer, where they can be found on the Monthly observations webpage under the heading of «SST».

If you all are correct, there will be an upward bias after 194x (where x is the end of WWII) and SST will still have an upward trend.

So, the next step will be to revisit the SST bias corrections and refine them, making use of the new information uncovered concerning national measurement practices and new analysis techniques that allow for more accurate corrections in areas and at times where there are few data.

This is particularly the case in areas where a change in SST causes the formation of fog, since much of the sea temperature change is taken up, not by a corresponding air temperature change, but by the condensation of water.

A Cess climate sensitivity parameter λ can then be computed as λ = ΔTs / ΔG, where Ts denotes global mean SST, G is TOA net radiative flux, and Δ indicates the difference between warming and present - day simulations»

In HadSST2 and earlier Met Office data sets, that's where the connection between NMAT and SST ended.