Sentences with phrase «ice ring using»

Not exact matches

Once all the cake is covered with rings of colorful icing begin to smooth out the frosting using an off - set spatula held perpendicular to your cake stand or spinner or turntable.

I forgot to mention that I used an ice cream scoop to scoop the batter into the rings.

Place about 1/3 cup (80 grams) of batter into each ring (I use an ice cream scoop).

Jack's pediatrician, José Enrique Clemente, finds it better for the child to «gum» ice rings / teethers or use oral analgesics (paracetamol).

The endeavor becomes more scientifically challenging in light of the large variety of information sources about past climate, including tree rings, coral, glacier ice, and marine and lake sediments, not to mention the complicated array of data that are used to establish the timelines that underlie the paleoclimate records.

On April 7, 2006, astronomers using the Keck Telescope announced that the outermost ring is bluish from sub-micronsized ice particles reflecting sunlight.

I forgot to mention that I used an ice cream scoop to scoop the batter into the rings.

necklace BaubleBar acrylic block monogram necklace in tortoise shell earrings Kendra Scott addie earrings in rose gold watch Michael Kors darci watch in gold bracelet c / o The Songbird Collection it bracelet in gold / The Songbird Collection small double triangle bracelet in gold — use code «jannadoan» or 20 % off rings Kendra Scott skylen ring in turqouise (sold out)-- similar but larger / BaubleBar tri bar ring (sold out) / BaubleBar ice chevron midi ring / Gorjana blakey ring cuff / Etsy stacking & midi rings lips MAC amplified creme lipstick in brick - o - la

The blob has a range of strange potions he can use, the blue warrior chick has some effective area denial tactics with ice walls, the suit of fiery armor is a damage spewing powerhouse from inside a ring of fire, and that cute little dragon... well, okay, he's the token nod to the series» inception as a tie - in to Spyro the Dragon.

I like this little dig at the denier - sceptic - contrarians who appear to be tree ring obsessed: «It is intriguing to note that the removal of tree - ring data from the proxy dataset yields less, rather than greater, peak cooling during the 16th — 19th centuries for both CPS and EIV methods... contradicting the claim... that tree - ring data are prone to yielding a warm - biased «Little Ice Age» relative to reconstructions using other high - resolution climate proxy indicators.»

The 78 - author paper, published Sunday in Nature Geoscience, used a variety of indirect indicators of temperature, from tree rings to pollen grains, to build on other work charting temperature shifts since the end of the last ice age — including the recent Marcott et al paper, explored here, which used seabed sediments to chart 11,000 years of temperatures.

My colleagues and I were using what we call proxy records, like corals and tree rings, and ice cores to try and extend the climate record back in time so that we could learn more about natural climate variability.

Proxies are used by paleoclimatologists and include ice cores, tree rings, lake sediments (varves), pollen counts, or anything that results from temperature or precipitation changes.

To answer the question of the Medieval Warm Period, more than 1,000 tree - ring, ice core, coral, sediment and other assorted proxy records spanning both hemispheres were used to construct a global map of temperature change over the past 1,500 years (Mann 2009).

The «hockey stick» describes a reconstruction of past temperature over the past 1000 to 2000 years using tree - rings, ice cores, coral and other records that act as proxies for temperature (Mann 1999).

There were no thermometers in 1000, so scientists use «proxy» data from items such as tree rings, lake sediments and ice cores.

The graph resulted from research by climatologists Michael Mann, Raymond Bradley, and Malcolm Hughes that used multiple proxies, including tree rings, coral, ice cores, sediments, and historical records.

But for years prior to that, scientists can only infer temperatures using what's called «proxies,» such as ice cores or tree rings, whose annual growth can be correlated with annual temperature variations.

Figure 1: Northern Hemisphere temperatures were reconstructed for the past 1000 years (up to 1999) using palaeoclimatic records (tree rings, corals, ice cores, lake sediments, etc.), along with historical and long instrumental records (WMO 2000).

In China, regional instrumental temperature series have been extended back over much of the past millennium using documentary data combined with inferences from ice cores and tree rings (Wang et al., 1998a, 1998b; Wang and Gong, 2000).

We can try to verify tree rings a lot further back than that, using ice cores as well as other proxies.

The most commonly used cosmogenic isotopes are radiocarbon (i.e., 14C) and 10Be, which are measured in tree - rings and in ice cores, respectively.

Five Weird Archives That Scientists Use to Study Past Climates When tree rings, ice cores, and cave formations can't cut it, try your luck with whale earwax or bat poop.

Interpretation of such proxy records of climate — for example, using tree rings to judge occurrence of droughts or gas bubbles in ice cores to study the atmosphere at the time the bubbles were trapped — is a well - established science that has grown much in recent years.

The second line of evidence is from reconstructions of past climates using evidence such as tree rings, ice cores, and corals.

I assume the error bars are cumulative — i.e., tree rings have a certain error bar, and ice cores have their error bars, and so do corals and lacustrine cores (I hope I used the right term there), and all of them add or multiply together (multiply, if I understand it correctly) when homogenizing and compiling them into one record.

Proxy data such as those generated from ice core samples, measurements of tree rings intervals, bore samples taken from sediments from the ocean and sea floor, and measurement of gases from bubbles trapped in ice are some examples of preserved physical characteristics of the past used by scientists to reconstruct prevailing climatic conditions in the past.

This is the time - span over which temperatures with annual resolution can be calculated using hemispheric - wide tree - ring, ice - cores, corals, and other annually - resolved proxy data.

These differences create annual layers in the ice that can be used to count the age of the ice, just like rings inside a tree.

In this study, more than 1000 tree - ring, ice core, coral, sediment and other assorted proxy records spanning both hemispheres were used to construct regional temperature change over the past 1500 years.

Using climate records culled from tree rings, glacial - ice layers and coral - growth layers, the three professors — whose research was funded in part by the federal government — determined in 1998 that temperatures have skyrocketed in the past century compared with the 500 years preceding it.

``, paleoclimatologists use measurements from tree rings, ice sheets, rocks, and other natural phenomena to estimate past temperature...»

Because Arctic sea ice is influenced by both air and water temperatures, the study authors use a combination of Arctic ice core, tree - ring and lake sediments to reconstruct Arctic conditions over the last 2,000 years.

It used corals, ice cores, tree rings, lake and [continue reading...]

The models have used measured data and reconstructed temperatures from proxies (tree rings, ice cores, boreholes, sediments, etc.) and been calibrated against at least the last few thousand years of data, and they all predict that the temperatures will continue to rise.

He and co-authors Ray Bradley and Malcolm Hughes used novel statistical techniques to extract more information than ever before from so - called «proxy records» — records of tree rings, ice cores, corals, and lake sediments — as well as «a smattering of historical [ie., written] records.»

Locations of proxy records with data back to AD 1000, 1500 and 1750 (instrumental: red thermometers; tree ring: brown triangles; borehole: black circles; ice core / ice borehole: blue stars; other including low - resolution records: purple squares) that have been used to reconstruct NH or SH temperatures by studies shown in Figure 6.10 (see Table 6.1, excluding O2005) or used to indicate SH regional temperatures (Figure 6.12).

Hegerl et al. (2006) used a mixture of 14 regional series, of which only 3 were not made up from tree ring data (a Greenland ice O isotope record and two composite series, from China and Europe, including a mixture of instrumental, documentary and other data).

Estimates of surface temperature changes further back in time must therefore make use of the few long available instrumental records or historical documents and natural archives or «climate proxy» indicators, such as tree rings, corals, ice cores and lake sediments, and historical documents to reconstruct patterns of past surface temperature change.

The lack of widespread instrumental climate records introduces the need for the use of natural climate archives from «proxy» data such as tree - rings, corals, speleothems and ice cores, as well as documentary evidence to reconstruct climate in past centuries (see Jones et al. 2009 for a review).

I have a feeling a lot of PhDs could get minted from extending your analysis here alone ---- does it hold for longer time series, using Vostok Ice Cores (not tree rings please!!)