Not exact matches
Researchers from the Niels Bohr Institute have analysed the natural
climate variations over the last 12,000
years, during which we have had a warm interglacial period and they have looked back 5 million
years to see the major features of the Earth's
climate.
«
Climate variations analyzed five million
years back in time.»
Using different calibration and filtering processes, the two researchers succeeded in combining a wide variety of available data from temperature measurements and
climate archives in such a way that they were able to compare the reconstructed sea surface temperature
variations at different locations around the globe on different time scales over a period of 7,000
years.
He and other scientists emphasized that this
year's 50 percent rebound stemmed from normal weather
variations, not an unusual
climate shift.
While the atmosphere is mainly causing
climate variations on shorter time scales, from months to
years, the longer - term fluctuations, such as those on decadal time scales, are primarily determined by the ocean.
While natural
climate variations like El Niño do affect the frequency and severity of heat waves from one
year to the next, the study suggests the increases are mainly linked to long - term changes in sea surface temperatures.
While most previous such work focuses on mean or average values, the authors in this paper acknowledge that
climate in the broader sense encompasses
variations between
years, trends, averages and extreme events.
Research published last
year by Professors Cox and Friedlingstein showed that these
variations in atmospheric carbon dioxide can reveal the sensitivity of tropical ecosystems to future
climate change.
Professor Cox, from the College of Engineering, Mathematics and Physical Sciences said «The
year - to -
year variation in carbon dioxide concentration is a very useful way to monitor how tropical ecosystems are responding to
climate.
It shows that while water in rivers and lakes would have disappeared as the
climate changed due to
variations in Earth's orbit, freshwater springs fed by groundwater could have stayed active for up to 1000
years without rainfall.
In a detailed study of more than 200
years» worth of temperature data, results backed previous findings that short - term pauses in
climate change are simply the result of natural
variation.
Although many technological improvements have been made to both grape growing and winemaking over the last few decades,
climate is often the wild card in determining
year - to -
year variations in quality.
The sediment cores used in this study cover a period when the planet went through many
climate cycles driven by
variations in Earth's orbit, from extreme glacial periods such as the Last Glacial Maximum about 20,000
years ago, when massive ice sheets covered the northern parts of Europe and North America, to relatively warm interglacial periods with
climates more like today's.
«According to our study, the Atlantic / Pacific temperature difference shows pronounced
variations on timescales of more than 5
years,» explained Chikamoto, USU associate professor in the department of Plants, Soils and
Climate.
The secret to the unique diversity of Lake Malawi's cichlid fish may be down to huge
variations in
climate and water levels over the
years
The changing
climate will enhance the wide
variations in weather that mid-latitude regions already experience from
year to
year and bring an increased number of extreme events such as heat waves and hailstorms, Busalacchi says.
«Remote cave study reveals 3000
years of European
climate variation.»
The team used a worldwide
climate model that incorporated normal month - to - month
variations in sea surface temperatures and sea ice coverage, among other
climate factors, to simulate 12,000
years» worth of weather.
«This is important for being able to predict
years of top - quality cava production, as well as for exploring the possible effects and
variations of
climate change on the quality» he concluded.
For example, El Niño and La Niña described above characterize
year - to -
year variations of
climate whereas the intra-seasonal time scale, discussed in our review article, bridges weather and
climate, i.e. 20 to 100 days.
2) A better ability to constrain
climate sensitivity from the past century's data 3) It will presumably be anticorrelated with
year to
year variations in global surface temperature that we see, especially from El Ninos and La Ninas, which will be nice whenever we have a cool
year and the deniers cry out «global warming stopped!».
About our estimates of the
climate transfer sensitivity to solar
variations at 11
years and 22
years, Dr. Benestad makes again a great confusion by misquoting and misunderstanding our paper.
In order to calculate the terrestrial response to more ephemeral solar
variations, S&W introduce another type of «
climate sensitivity» which they calculate separately for each of two components representing frequency ranges 7.3 - 14.7 and 14.7 - 29.3
year ranges respectively.
in the other case, another friend made disparaging remarks about my cfl's and when i later said, very casually, something to the effect that he doubted the science, he referred to something dixie lee ray said at least fifty
years ago about ice ages and
climate variations.
Although droughts have been a natural part of the
year - to -
year variations in the Amazon's
climate, both the frequency and severity of droughts in the rainforest have been increasing over the last decade because of
climate change, Aragão says:
The presented range though does not correlate with an analogical temperature range constructed for the
years 1068 - 1979 in Europe according to biological and documentary data (Guiot, J.: The combination of historical documents and biological data in the reconstruction of
climate variations in space and time.
Periods of volcanism can cool the
climate (as with the 1991 Pinatubo eruption), methane emissions from increased biological activity can warm the
climate, and slight changes in solar output and orbital
variations can all have
climate effects which are much shorter in duration than the ice age cycles, ranging from less than a decade to a thousand
years in duration (the Younger Dryas).
Over the last 30
years of direct satellite observation of the Earth's
climate, many natural influences including orbital
variations, solar and volcanic activity, and oceanic conditions like El Nino (ENSO) and the Pacific Decadal Oscillation (PDO) have either had no effect or promoted cooling conditions.
Understanding how such
year - to -
year natural
climate variations impact coastal water levels is key to developing a full picture of the sea level rise threat through the end of the century.
«
Climate models show that ice - sheet melt will dominate sea - level rise over the coming centuries, but our understanding of ice - sheet
variations before the last interglacial 125,000
years ago remains fragmentary.
His research concerns understanding global
climate and its
variations using observations and covers the quasi biennial oscillation, Pacific decadal oscillation and the annular modes of the Arctic oscillation and the Antarctic oscillation, and the dominant spatial patterns in month - to - month and
year - to -
year climate variability, including the one through which El Niño phenomenon in the tropical Pacific influences
climate over North America.
Multiple variables, from
climate variations to the presence of wildlife carriers, cause rates of infections to vary dramatically from
year to
year — even within communities.
Although there are pronounced wet and dry seasons as well as
variations between the interior
climate and the
climate along the coast, Belize boasts amazing warm temperatures every month of the
year.
Climate is mild, with little
variation in temperature
year round.
Just like the rest of Fiji, Viti Levu has a tropical
climate, meaning that the weather is nearly always warm and there is little seasonal
variation in temperature throughout the
year.
Climate change involves time scales of many
years, and hence if emphasis is given to much shorter time scales, the trends will drown in noisy
variations.
But you can look at past
climate records, and see no sign, over many thousands of
years, that solar
variations have had effects of anything like the size needed to cancel out the expected effects of increased greenhouse gas levels in the atmosphere over the next few decades.
It is to be noted here that there is no necessary contradiction between forecast expectations of (a) some renewed (or continuation of) slight cooling of world
climate for a few decades to come, e.g., from volcanic or solar activity
variations; (b) an abrupt warming due to the effect of increasing carbon dioxide, lasting some centuries until fossil fuels are exhausted and a while thereafter; and this followed in turn by (c) a glaciation lasting (like the previous ones) for many thousands of
years.»
2) A better ability to constrain
climate sensitivity from the past century's data 3) It will presumably be anticorrelated with
year to
year variations in global surface temperature that we see, especially from El Ninos and La Ninas, which will be nice whenever we have a cool
year and the deniers cry out «global warming stopped!».
Mike's work, like that of previous award winners, is diverse, and includes pioneering and highly cited work in time series analysis (an elegant use of Thomson's multitaper spectral analysis approach to detect spatiotemporal oscillations in the
climate record and methods for smoothing temporal data), decadal climate variability (the term «Atlantic Multidecadal Oscillation» or «AMO» was coined by Mike in an interview with Science's Richard Kerr about a paper he had published with Tom Delworth of GFDL showing evidence in both climate model simulations and observational data for a 50 - 70 year oscillation in the climate system; significantly Mike also published work with Kerry Emanuel in 2006 showing that the AMO concept has been overstated as regards its role in 20th century tropical Atlantic SST changes, a finding recently reaffirmed by a study published in Nature), in showing how changes in radiative forcing from volcanoes can affect ENSO, in examining the role of solar variations in explaining the pattern of the Medieval Climate Anomaly and Little Ice Age, the relationship between the climate changes of past centuries and phenomena such as Atlantic tropical cyclones and global sea level, and even a bit of work in atmospheric chemistry (an analysis of beryllium - 7 measure
climate record and methods for smoothing temporal data), decadal
climate variability (the term «Atlantic Multidecadal Oscillation» or «AMO» was coined by Mike in an interview with Science's Richard Kerr about a paper he had published with Tom Delworth of GFDL showing evidence in both climate model simulations and observational data for a 50 - 70 year oscillation in the climate system; significantly Mike also published work with Kerry Emanuel in 2006 showing that the AMO concept has been overstated as regards its role in 20th century tropical Atlantic SST changes, a finding recently reaffirmed by a study published in Nature), in showing how changes in radiative forcing from volcanoes can affect ENSO, in examining the role of solar variations in explaining the pattern of the Medieval Climate Anomaly and Little Ice Age, the relationship between the climate changes of past centuries and phenomena such as Atlantic tropical cyclones and global sea level, and even a bit of work in atmospheric chemistry (an analysis of beryllium - 7 measure
climate variability (the term «Atlantic Multidecadal Oscillation» or «AMO» was coined by Mike in an interview with Science's Richard Kerr about a paper he had published with Tom Delworth of GFDL showing evidence in both
climate model simulations and observational data for a 50 - 70 year oscillation in the climate system; significantly Mike also published work with Kerry Emanuel in 2006 showing that the AMO concept has been overstated as regards its role in 20th century tropical Atlantic SST changes, a finding recently reaffirmed by a study published in Nature), in showing how changes in radiative forcing from volcanoes can affect ENSO, in examining the role of solar variations in explaining the pattern of the Medieval Climate Anomaly and Little Ice Age, the relationship between the climate changes of past centuries and phenomena such as Atlantic tropical cyclones and global sea level, and even a bit of work in atmospheric chemistry (an analysis of beryllium - 7 measure
climate model simulations and observational data for a 50 - 70
year oscillation in the
climate system; significantly Mike also published work with Kerry Emanuel in 2006 showing that the AMO concept has been overstated as regards its role in 20th century tropical Atlantic SST changes, a finding recently reaffirmed by a study published in Nature), in showing how changes in radiative forcing from volcanoes can affect ENSO, in examining the role of solar variations in explaining the pattern of the Medieval Climate Anomaly and Little Ice Age, the relationship between the climate changes of past centuries and phenomena such as Atlantic tropical cyclones and global sea level, and even a bit of work in atmospheric chemistry (an analysis of beryllium - 7 measure
climate system; significantly Mike also published work with Kerry Emanuel in 2006 showing that the AMO concept has been overstated as regards its role in 20th century tropical Atlantic SST changes, a finding recently reaffirmed by a study published in Nature), in showing how changes in radiative forcing from volcanoes can affect ENSO, in examining the role of solar
variations in explaining the pattern of the Medieval
Climate Anomaly and Little Ice Age, the relationship between the climate changes of past centuries and phenomena such as Atlantic tropical cyclones and global sea level, and even a bit of work in atmospheric chemistry (an analysis of beryllium - 7 measure
Climate Anomaly and Little Ice Age, the relationship between the
climate changes of past centuries and phenomena such as Atlantic tropical cyclones and global sea level, and even a bit of work in atmospheric chemistry (an analysis of beryllium - 7 measure
climate changes of past centuries and phenomena such as Atlantic tropical cyclones and global sea level, and even a bit of work in atmospheric chemistry (an analysis of beryllium - 7 measurements).
But it's like I say: as planetary
climate systems show all possible signs of disruption, what we get is strange climatic conditions and extreme weather events on a local level, and these conditions and event are conditioned by great
variations from continent to continent and from one
year to the next.
tpinlb,
climate models don't «predict»
year - specific phenomena arising from stochastic
variation that adds «noise» to progression of
climate states under the influence of persistent forcings.
Large changes in cosmic rays are documented in response to magnetic - field
variations (the Laschamp event of about 40,000
years ago is especially prominent) with no corresponding change in
climate, so any cosmic - ray influence on the
climate must be very small (a weak correlation can be obscured by noise; a strong control is almost always visible «by eye,» and clearly is absent).
Jeff Tollefson, in Nature (http://www.nature.com/news/
climate-change-the-case-of-the-missing-heat-1.14525): «For several
years, scientists wrote off the stall as noise in the
climate system: the natural
variations in the atmosphere, oceans and biosphere that drive warm or cool spells around the globe.
How is it then possible that the IPCC
climate models can replicate these decadal
variations at exactly the same
years?
Tad (215), there have been a couple papers come out in the last
year that place the Australian drought in the context of natural
variation and global
climate change:
When Indian leaders and, by extension, news media, address
climate change they frequently invoke some
variation on the «per capita principle» — Prime Minister Manmohan Singh's vow that India's per - capita greenhouse gas emissions — just above one ton per
year — will never exceed the West's.
«What is generally required [for proving solar forcing of
climate change] is a consistent signal over a number of cycles (either the 11
year sunspot cycle or more long term
variations), similar effects if the timeseries are split, and sufficient true degrees of freedom that the connection is significant and that it explains a non-negligible fraction of the variance.»
«Today, scientists who study the links between solar activity and
climate are confident that the small
variations in TSI associated with the eleven -
year solar cycle can not explain the intensity and speed of warming trends seen on Earth during the last century.
Climate is notoriously «noisy», so it typically takes > 15
years to make out a trend of the current size of the global warming trend inside the typical interannual
variation.