Sentences with phrase «for regional warming»
But the latest study suggests that aerosols can be responsible for regional warming.
https://news.nationalgeographic.com/ Not exact matches
Every Grain of Rice — authentic Chinese home - cooking Breakfast for Dinner — sweet and savory breakfast combinations re-purposed for dinnertime The Little Paris Kitchen — classic French cooking made simple enough for every day by TV star Rachel Khoo Sicilia in Cucina — gorgeous, dual - language cookbook focused on the regional flavors of Sicily Venezia in Cucina — sister book to Sicilia in Cucina, but focused on Venice Vegetable Literacy — highly informative vegetable cookbook / encyclopedia, a great resource for enthusiastic kitchen gardeners The Chef's Collaborative — creative recipes from a number of chefs celebrating local, seasonal produce Home Made Summer — a sequel to Home Made and Home Made Winter, packed with simple, summery recipes that make the most of the season's bounty Try This At Home — a fun introduction to molecular gastronomy techniques through the ever creative eyes of Top - Chef Winner Richard Blais Cooking with Flowers — full of sweet recipes that can be made from the flowers in your neighborhood, like lilacs, marigolds, and daylilies Vegetarian Everyday — healthy, creative recipes from the couple behind Green Kitchen Stories The Southern Vegetarian — favorite Southern comfort food classics turned vegetarian by the folks at The Chubby Vegetarian Le Pain Quotidien — simple soups, salads, breads, and desserts from the well - loved Belgian chain Live Fire — ambitious live - fire cooking projects that range from roasting an entire lamb on an iron cross to stuffing burgers with blue cheese to throw on your grill True Brews — a great, accessible introduction to brewing your own soda, kombucha, kefir, cider, beer, mead, sake, and fruit wine Le Petit Paris — a cute little book of classic sweet and savory French dishes, miniaturized for your next cocktail party Wild Rosemary & Lemon Cake — regional Italian cookbook focused on the flavors of the Amalfi coast Vedge — creative, playful vegan recipes from Philadelphia's popular restaurant of the same Full of Flavor — a whimsical cookbook that builds intense flavor around 18 key ingredients Le Pigeon — ambitious but amazing recipes for cooking meat of all sorts, from lamb tongue to eel to bison Pickles, Pigs, and Whiskey — a journey through Southern food in many forms, from home pickling and meat curing to making a perfect gumbo Jenny McCoy's Desserts for Every Season — gorgeous, unique desserts that make the most of each season's best fruits, nuts, and vegetables Winter Cocktails — warm toddies, creamy eggnogs, festive punches, and everything else you need to get you through the colder months Bountiful — produce - heavy, garden - inspired recipe from Diane and Todd of White on Rice Couple Melt — macaroni and cheese taken to extremes you would never have thought of, in the best way possible The Craft Beer Cookbook — all your favorite comfort food recipes infused with the flavors of craft beers, from beer expert Jackie of The Beeroness
From large urban healthcare campuses to smaller regional medical centers, Towne Health has been providing warm welcomes and safe departures from coast to coast for over two decades.
If the onset of maturity comes earlier in the season, it means that grapes ripen during a warmer period — affecting sugar levels, aromas and flavors and changing the unique identity that connoisseurs look for in regional wines.
The research concludes that for other changes, such as regional warming and sea ice changes, the observations over the satellite - era since 1979 are not yet long enough for the signal of human - induced climate change to be clearly separated from the strong natural variability in the region
They also conclude that regional precipitation projections for warming of 1.5 degrees C and 2 degrees C remain uncertain, «but the eastern U.S. is projected to experience wetter winters and the Great Plains and Northwest are projected to experience drier summers in the future.»
Tuna, marlin and great white sharks heat up certain areas — swimming muscles, parts of their viscera and the eye and brain — but these regional endotherms can stay at lower depths only for short periods and must rise to warmer waters, unlike the deep - dwelling opah.
The U.S. press is either woefully ignorant of the state of the science, or is deliberately trying to find explanations for various regional weather and climate changes that don't involve any mention of «global warming» — and that approach relies on the «natural cycle» argument.
These are based on observations of regional change around the South Polar Cap, but seem to have been extended into a «global» change, and used by some to infer an external common mechanism for global warming on Earth and Mars (e.g. here and here).
Naturally occurring interannual and multidecadal shifts in regional ocean regimes such as the Pacific El Niño - Southern Oscillation, the North Atlantic Oscillation, and the Atlantic Multidecadal Oscillation, for example, are bimodal oscillations that cycle between phases of warmer and cooler sea surface temperatures.
«And the regional information is critical for climate forecasts and understanding future global warming impacts.»
Finally, our simulated AOA for 2020 — 2100 in the RCP2.6 scenario is capable of offsetting warming and ameliorating ocean acidification increases at the global scale, but with highly variable regional responses.
Specificaly, we were talking about a regional warming event in the context of an otherwise unremarkable month for «Global» temperatures.
Evidence for regional warmth during medieval times can be found in a diverse but more limited set of records including ice cores, tree rings, marine sediments, and historical sources from Europe and Asia, but the exact timing and duration of warm periods may have varied from region to region, and the magnitude and geographic extent of the warmth are uncertain.
The older Met Office Hadley Centre model, HadCM3, (in) famously produced an emergent result of very substantial drying and warming in the Amazon, taking the regional climate below the threshold for which rainforest could be supported.
The Gettys BLU team tapped into their collective knowledge of regional practices, processes and expectations to create a warm and welcoming environment filled with thoughtful amenities and opportunities for relaxation and indulgence.
Steeped in centuries of holiday traditions, these epicenters of good cheer feature hundreds of vendors selling everything from regional handicrafts, to local delicacies and sweets, warm wine (it's amazing), hot cocoa, and so many wacky and interesting gifts for friends and family back home that you'll need another travel backpack.
Its 100 exquisitely designed accommodations feature the largest over-water villas in the South Seas as well as stunning beach villas, showcases for the warm glow of exotic woods, handwoven fabrics and regional art.
Admired for her keen eye and warm personality, she has been a crucial supporter of Atlanta and regional artists.
However, there are various other plausible explanations, for example: — changes in US temperatures since the 1930s / 1940s show regional variation within the overall warming trend at those latitudes; — actually I'm struggling to think of any others, apart from inaccuracies in the US temperature record but these have tended to point the other way.
Ranked warmest years in the series going back to 1914 are: # 2006 9.73 °C # 2003 9.51 °C # 2004 9.48 °C # 2002 9.48 °C # 2005 9.46 °C Mean temperature, sunshine and rainfall for regions of the UK compared with the long - term average UK regional averages for 2006, anomalies with respect to 1971 - 2000 Region Mean temp Sunshine Rainfall Actual [°C] Anom [°C] Actual [hours] Anom [%] Actual [mm] Anom [%] UK 9.7 +1.1 1,507 113 1,176 104 England 10.6 +1.2 1,638 112 8,51 102 Wales 9.9 +1.0 1,534 113 1,420 99 Scotland 8.3 +1.1 1,300 112 1,652 109 N Ireland 9.6 +1.0 1,409 115 1,156 104
4) Autumn and winter temperatures will increase by a regional average of 4 °C over the next 30 years — twice the warming projected for the Northern Hemisphere as a whole --
This is the linchpin: if the difference between pre-industrial and modern temperatures is not as dramatic as this analysis indicates — i.e. if modern GLOBAL temperatures are comparable to those of the Medieval Warm Period (named for a REGIONAL phenomenon)-- then there is little need for urgency.
These are based on observations of regional change around the South Polar Cap, but seem to have been extended into a «global» change, and used by some to infer an external common mechanism for global warming on Earth and Mars (e.g. here and here).
TreeHugger has noted, somewhat light - heartedly, that among the myriad effects of global warming are likely reductions in wine and beer production; as global warming alters the planet's regional climates, it affects the crop yields used for brewing up our favorite libations.
Evidence for regional warmth during medieval times can be found in a diverse but more limited set of records including ice cores, tree rings, marine sediments, and historical sources from Europe and Asia, but the exact timing and duration of warm periods may have varied from region to region, and the magnitude and geographic extent of the warmth are uncertain.
The climate scientists behind the report are less ready, however, to predict what the specific impacts of global warming will look like in the coming decades, meaning it won't be very useful for regional planners.
The large warming trend during the period is due to a regime shift in around 1988, which accounted for about 51 % of the regional warming.
As this NOAA / NCDC regional climate map reveals, the vast majority of the continental U.S. has not warmed for the last 15 calendar years.
Yet, we explained there is also reasonable basis for concern that a warming world may at least temporarily increase tornado damage including the fact that oceans are now warmer, and regional ocean circulation cycles such as La Nina / El Nino patterns in the Pacific which affect upper atmospheric conditions appear to becoming more chaotic under the influence of climate change.
-- Susan Solomon, Nature The Long Thaw is written for anyone who wishes to know what cutting - edge science tells us about the modern issue of global warming and its effects on the pathways of atmospheric chemistry, as well as global and regional temperatures, rainfall, sea level, Arctic sea - ice coverage, melting of the continental ice sheets, cyclonic storm frequency and intensity and ocean acidification.
Global mean losses could be 1 to 5 % of GDP for 4 °C of warming, but regional losses could be substantially higher.
Their results highlight the possibility of a strong precipitation reduction in the northern edge of the monsoon in response to warming, with consequences for regional water resources, agriculture and ecosystems.
The authors conclude that the there is a higher retreat - rate for marine terminating glaciers in the recent warm period; in the 1930s when there is a natural mode of variability active that caused regional temperatures around Greenland to be anomalously warm, there was a higher retreat rate for land - terminating glaciers (the lower retreat rate today is in part because they are currently smaller).
Furthermore, Siberia would be one of the regions for which climate change would indeed be a regional warming - it is already heating up [wikipedia.org] much faster than any other part of the globe, and if it keeps doing so, it will become much more prospective for human settlement and agriculture, and in short - term perspective provide for easier access to the vast natural resources of the region.
For example, Kosaka and Xie showed than when the El Niño - related changes in Pacific ocean temperature are entered into a model, it not only reproduced the global surface warming over the past 15 years but it also accurately reproduced regional and seasonal changes in surface temperatures.
Mosher, why on your poster with Zeke, do the different methodologies for estimating the average temperature of the CUS give the same history, and yet the regional levels of warming and cooling are quite different?
I predict they will mutate the argument, and with a completely straight face — the effect of carbon dioxide will turn out to be «more complicated», scientists will rediscover that the molecule emits infra red too — and now rather than just simple warming, it will be responsible for «transforming regional patterns», «shifting layers» and «wandering jet streams».
I found it too dry and wanted to work in the Environment, where global warming has always been a background to my work but not the focus except for a year where I ran regional climate models.
Owing to the decreased number of spatial degrees of freedom in the earliest reconstructions (associated with significantly decreased calibrated variance before e.g. 1730 for annual - mean and cold - season, and about 1750 for warm - season pattern reconstructions) regional inferences are most meaningful in the mid 18th century and later, while the largest - scale averages are useful further back in time.
On a regional basis for clear - sky daytime conditions, conversion of natural vegetation to a crop / pasture mosaic warms the cerrado by an average of 1.55 °C, but subsequent conversion of that mosaic to sugar cane cools the region by an average of 0.93 °C (1.67 °F), resulting in a mean net increase of 0.6 °C.
In addition, the pattern of sea surface temperatures at low latitudes is extremely important for regional climate variations (shown, for example, by the increased likelihood of heavy winter rainfall in California when the eastern tropical Pacific warms in El Niño events).
As the global climate warms, at - risk communities need to improve governance of wildfire issues, including landscape management, while also strengthening regional and international measures for cooperation, Goldammer tells Pacific Standard.
None of these observations by themselves prove the world is warming; they could simply be regional effects, for instance.
about 7 - 12 % / The Arctic warming in 1920 - / Global Change and Ecosystems GLOBAL CHANGE AND ECOSYSTEMS Specific Support Actions SECOND CALL u Actions such as the European Network for Research and Global Change (ENRICH) u Actions for associated candidate countries u European contribution to climate related / relating to regional and urban sustainability aspects E u r o p e a n C o m m i s s i o nCommunity Research Global Change and Ecosystems 3rd Call for Proposals (16 June 2004) Climate research topics /
To point out just a couple of things: — oceans warming slower (or cooling slower) than lands on long - time trends is absolutely normal, because water is more difficult both to warm or to cool (I mean, we require both a bigger heat flow and more time); at the contrary, I see as a non-sense theory (made by some serrist, but don't know who) that oceans are storing up heat, and that suddenly they will release such heat as a positive feedback: or the water warms than no heat can be considered ad «stored» (we have no phase change inside oceans, so no latent heat) or oceans begin to release heat but in the same time they have to cool (because they are losing heat); so, I don't feel strange that in last years land temperatures for some series (NCDC and GISS) can be heating up while oceans are slightly cooling, but I feel strange that they are heating up so much to reverse global trend from slightly negative / stable to slightly positive; but, in the end, all this is not an evidence that lands» warming is led by UHI (but, this effect, I would not exclude it from having a small part in temperature trends for some regional area, but just small); both because, as writtend, it is normal to have waters warming slower than lands, and because lands» temperatures are often measured in a not so precise way (despite they continue to give us a global uncertainity in TT values which is barely the instrumental's one)-- but, to point out, HadCRU and MSU of last years (I mean always 2002 - 2006) follow much better waters» temperatures trend; — metropolis and larger cities temperature trends actually show an increase in UHI effect, but I think the sites are few, and the covered area is very small worldwide, so the global effect is very poor (but it still can be sensible for regional effects); but I would not run out a small warming trend for airport measurements due mainly to three things: increasing jet planes traffic, enlarging airports (then more buildings and more asphalt — if you follow motor sports, or simply live in a town / city, you will know how easy they get very warmer than air during day, and how much it can slow night - time cooling) and overall having airports nearer to cities (if not becoming an area inside the city after some decade of hurban growth, e.g. Milan - Linate); — I found no point about UHI in towns and villages; you will tell me they are not large cities; but, in comparison with 20-40-60 years ago when they were «countryside», many small towns and villages have become part of larger hurban areas (at least in Europe and Asia) so examining just larger cities would not be enough in my opinion to get a full view of UHI effect (still remembering that it has a small global effect: we can say many matters are due to UHI instead of GW, maybe even that a small part of measured GW is due to UHI, and that GW measurements are not so precise to make us able to make good analisyses and predictions, but not that GW is due to UHI).
Ruff, T. W. and J. D. Neelin (2012), Long tails in regional surface temperature probability distributions with implications for extremes under global warming, Geophys.
Confirming evidence for evporation negating the warming effect of CO2 is look at regional warming.
Though there can be significant differences in regional surface impacts between one SSW event and another, the typical pattern includes changes in sea level pressure resembling the negative phase of the North Atlantic Oscillation (NAO) / Arctic Oscillation (AO), (representing a southward shift in the Atlantic storm track), wetter than average conditions for much of Europe, cold air outbreaks throughout the mid-latitudes, and warmer than average conditions in eastern Canada and subtropical Asia (see figure below, left panel).
Stenchikov et al. (2006) showed that models have difficulty in capturing the regional response of the climate system (ao) to Volcanic singularities specifically the temperature regime in eurasia in the Giss model, or in retrodiction ie the Krakatoa problem why was it so warm, thus there is no uniqueness theorem for volcanics.