Hence, studies of
observed changes in regions influenced by an oscillation may be able to attribute these changes to regional climate variations, but decades of data may be needed in order to separate the response to climate oscillations from that due to longer - term climate change.
What's most intriguing is what is causing the dramatically warm waters — and how this may relate to other
observed changes in the region.
Not exact matches
Jesus would say that all that great host do not belong to him... they are an offended bunch for whatever
region... if you were to
observe Christianity through all those four forms you would
change your mind and say that all Christians should strive to be what Jesus said of the good ground... good Christians
in that parable are out numbered 3 to 1...
The data, collected by aerial survey missions flown
in the Southern Hemisphere
in the summer of 2014 - 2015, provide detailed topography of the perpetually ice - free
region, where surprising landscape
changes, such as rapid erosion along some streams, have been
observed in recent years.
In particular, the modelers could now reproduce in detail the pattern of warming, changes in rainfall, etc. actually observed in different regions of the world over the past centur
In particular, the modelers could now reproduce
in detail the pattern of warming, changes in rainfall, etc. actually observed in different regions of the world over the past centur
in detail the pattern of warming,
changes in rainfall, etc. actually observed in different regions of the world over the past centur
in rainfall, etc. actually
observed in different regions of the world over the past centur
in different
regions of the world over the past century.
To see how increased temperatures might contribute to the reductions
in the river's flow that have been
observed since 2000, Udall and Overpeck reviewed and synthesized 25 years of research about how climate and climate
change have and will affect the
region and how temperature and precipitation affect the river's flows.
Taking factors such as sea surface temperature, greenhouse gases and natural aerosol particles into consideration, the researchers determined that
changes in the concentration of black carbon could be the primary driving force behind the
observed alterations to the hydrological cycle
in the
region.
The research has also contributed to answering the important question whether the increase
in rainfall
observed in the tropics was simply caused by the fact of a warmer atmosphere or whether the underlying circulation
in that
region had
changed.
«Eavesdropping on Bering Strait marine mammals: Researchers are eavesdropping on marine mammals within the Bering Strait via «passive acoustic monitoring» to
observe changes in the ecology of the Pacific Arctic by documenting the use of this
region by species previously excluded by sea ice.»
The
changes in these
regions can account for about 90 percent of the
observed variation
in the river's streamflow over the last century, with one to four months lead - time.
The assessment describes effects of climate
change that have already been
observed; projected
changes in the climate and the landscape; and forest vulnerabilities
in a 23.5 - million - acre
region of forest
in northeastern Minnesota.
In the present work, physicist Patrick Schuenke and physician and physicist Daniel Paech have been able to observe the changes of glucose signals in healthy brain regions as well as pathogenic changes in human brain cance
In the present work, physicist Patrick Schuenke and physician and physicist Daniel Paech have been able to
observe the
changes of glucose signals
in healthy brain regions as well as pathogenic changes in human brain cance
in healthy brain
regions as well as pathogenic
changes in human brain cance
in human brain cancer.
Although this
region is far too deep for researchers to ever
observe directly, instruments that can measure the propagation of seismic waves caused by earthquakes allow them to visualize
changes in Earth's interior structure; similar to how ultrasound measurements let medical professionals look inside of our bodies.
Scientists are still only just beginning to understand the myriad mechanisms that control the seemingly dramatic melting
observed in regions of West Antarctica, and how climate
change is affecting all the moving parts.
Thus the study shows that that iRAM simulates recently
observed cloud cover
changes in this the eastern Pacific more accurately than the GCMs, and iRAM also successfully simulates the main features of the
observed interannual variation of clouds
in this
region, including the evolution of the clouds through the El Niño Southern Oscillation (ENSO) cycle.
Consistent with
observed changes in surface temperature, there has been an almost worldwide reduction
in glacier and small ice cap (not including Antarctica and Greenland) mass and extent
in the 20th century; snow cover has decreased
in many
regions of the Northern Hemisphere; sea ice extents have decreased
in the Arctic, particularly
in spring and summer (Chapter 4); the oceans are warming; and sea level is rising (Chapter 5).
POLENET (The Polar Earth
Observing Network) is a global network dedicated to observing the polar regions in a changi
Observing Network) is a global network dedicated to
observing the polar regions in a changi
observing the polar
regions in a
changing world.
b shows
regions that have experienced
changes in the frequency of long fire weather seasons (> 1σ above historical mean) during the second half of the study period (1996 — 2013) compared with the number of events
observed during the first half (1979 — 1996).
Based on these observations and experiments, Harker and Pevtsov conclude that the
observed magnetic transient is not an artifact created by the SDO / HMI observation process, but instead represents a real
change in the vector magnetic field; since the active
region was located so close to the solar limb, this suggests that the transient manifested
in the horizontal component of the magnetic field (relative to the solar surface).
But with recent advances
in technology, we can now
observe regions changing over time, for a deeper understanding of how stars form.
In addition to its descending outputs, the PPN has ascending connections to the neocortex, either directly or indirectly via the thalamus, and so pathological changes in this region may be partly responsible for the cognitive disorders of aging or those observed in various neurodegenerative condition
In addition to its descending outputs, the PPN has ascending connections to the neocortex, either directly or indirectly via the thalamus, and so pathological
changes in this region may be partly responsible for the cognitive disorders of aging or those observed in various neurodegenerative condition
in this
region may be partly responsible for the cognitive disorders of aging or those
observed in various neurodegenerative condition
in various neurodegenerative conditions.
This is further compounded by elevations
in metabolic efficiency (whereby energy expenditure declines beyond that predicted from the
change in metabolic mass) and appetite which accompany weight - loss, and may ultimately predispose to weight re - gain.82 Moreover,
changes in neural activity within brain
regions known to be involved
in regulatory, emotional and cognitive control of food intake have also been
observed following weight - loss.83
It is possible that the different regional hypertrophy
observed after training at long or short muscle lengths could
in fact be closely related to the
changes in muscle fascicle length, because
changes in muscle fascicle length have been linked to greater increases
in muscle size
in the distal
regions of the muscle (Franchi et al. 2014).
The U.S. Global
Change Research Program, composed of 13 federal agencies, reported
in 2009 that climate - related
changes are already being
observed in every
region of the world, including the United States and its coastal waters.
The workshop focused on linking these fields to better understand how
changes observed in the cryosphere affect lakes and streams
in mountain
regions.
The
observed temperature
change is
in the
region of just under 0.7 °C (1.3 °F) with errors of ± 0.05 °C (± 0.1 °F).
climate - related
changes are already being
observed in every
region of the world, including the United States and its coastal waters.
For the entire Northern Hemisphere, there is evidence of an increase
in both storm frequency and intensity during the cold season since 1950,1 with storm tracks having shifted slightly towards the poles.2, 3 Extremely heavy snowstorms increased
in number during the last century
in northern and eastern parts of the United States, but have been less frequent since 2000.11,15 Total seasonal snowfall has generally decreased
in southern and some western areas, 16 increased
in the northern Great Plains and Great Lakes
region, 16,17 and not
changed in other areas, such as the Sierra Nevada, although snow is melting earlier
in the year and more precipitation is falling as rain versus snow.18 Very snowy winters have generally been decreasing
in frequency
in most
regions over the last 10 to 20 years, although the Northeast has been seeing a normal number of such winters.19 Heavier - than - normal snowfalls recently
observed in the Midwest and Northeast U.S.
in some years, with little snow
in other years, are consistent with indications of increased blocking (a large scale pressure pattern with little or no movement) of the wintertime circulation of the Northern Hemisphere.5 However, conclusions about trends
in blocking have been found to depend on the method of analysis, 6 so the assessment and attribution of trends
in blocking remains an active research area.
This technical document explores available data on the
observed and projected linkages between climate
change and health
in the Asia - Pacific
region.
«Climate data coverage remains limited
in some
regions and there is a notable lack of geographic balance
in data and literature on
observed changes in natural and managed systems, with marked scarcity
in developing countries.
Maya Sherpa, a 35 - year - old mountaineer from Okhaldhunga district, said they
observed the impacts of climate
change in the high Himalayan
region during their K2 expedition.
«
In my decade - long career in mountaineering so far, I have observed noticeable changes in weather patterns of the high Himalayan region,» said Pasang Lhamu, a 30 - year - old mountaineer from Solukhumbu distric
In my decade - long career
in mountaineering so far, I have observed noticeable changes in weather patterns of the high Himalayan region,» said Pasang Lhamu, a 30 - year - old mountaineer from Solukhumbu distric
in mountaineering so far, I have
observed noticeable
changes in weather patterns of the high Himalayan region,» said Pasang Lhamu, a 30 - year - old mountaineer from Solukhumbu distric
in weather patterns of the high Himalayan
region,» said Pasang Lhamu, a 30 - year - old mountaineer from Solukhumbu district.
A method of dealing with the lack of mass balance measurements is to estimate the
changes in mass balance as a function of climate, using mass balance sensitivities (see Box 11.2 for definition) and
observed or modelled climate
change for glacier covered
regions.
The overall glacier
change behaviors are similar to glaciers
observed in other part of the Himalayan
region.
The table that accompanies the above passage from the IPCC's report, captioned «Extreme weather and climate events: global - scale assessment of recent
observed changes, human contribution to the
changes, and projected further
changes for the early (2016 — 2035) and late (2081 — 2100) 21 st century `'» has the following entries for «Increases
in intensity and / or duration of drought»: under
changes observed since 1950, «low confidence on a global scale, likely
changes in some
regions `'» [emphasis added]; and under projected
changes for the late 21 st century, «likely (medium confidence) on a regional to global scale».
Larger - scale aggregation offers insights into the relationships between the
observed changes assessed
in Section 1.3 and temperature, by combining results from many studies over multiple systems and larger
regions.
(I have always been careful to note that, scientifically, we can not say that climate
change caused a particular drought, but only that it is expected to increase the frequency, intensity, and duration of drought
in some
regions, and that such
changes are being
observed.)
Average precipitation is
changing in many
regions with both increases and decreases and there is a general tendency for increases
in extreme precipitation
observed over land areas.
There is increasing evidence that farmers
in some
regions are already adapting to
observed climate
changes in particular altering cultivation and sowing times and crop cultivars and species.
(d) Scherhag stressed: «such kind of climate
changes as could now be
observed in Spitsbergen and along the western coast of Greenland were certainly not restricted to a small
region but must be global» (Scherhag, 1937).
Slow variations
in upper ocean heat content that have been
observed in the subpolar and marginal ice zone
regions of the Atlantic since the mid-twentieth century are thought to be related to
changes in the strength of the Atlantic Meridional Overturning Circulation (AMOC).
The new research uses multiple runs of a coupled ocean - atmosphere computer model to simulate global temperature
changes in response to climate forcing when the sea surface temperature (SST)
in the el Niño
region follows its historically
observed values.
Summary of estimated impacts of
observed climate
changes on yields over 1960 - 2013 for four major crops
in temperate and tropical
regions.
Tree mortality has been
observed to increase over the past decades
in many
regions, but the causes of this increase are not well understood, and we know even less about long - term
changes in growth and recruitment rates.
The pace and magnitude of the
changes observed in this
region match the expectation that Amundsen Sea embayment glaciers should be less stable than others.
Observed bleaching
in response to warm tropical waters invading cooler
regions aroused fears that climate
change had contributed to this «unprecedented» event.
It appears that moderate levels of atmospheric CO2 rise and climate
change relative to current conditions may be beneficial
in some
regions (Nemani et al., 2003), depending on latitude, on the CO2 responsiveness of plant functional types, and on the natural adaptive capacity of indigenous biota (mainly through range shifts that are now being widely
observed — see Chapter 1).
Anthropogenic influences have contributed to
observed increases
in atmospheric moisture content
in the atmosphere (medium confidence), to global - scale
changes in precipitation patterns over land (medium confidence), to intensification of heavy precipitation over land
regions where data are sufficient (medium confidence), and to
changes in surface and subsurface ocean salinity (very likely).
The
observed pattern of ocean temperature
change created a propensity for drought
in some
regions around the globe — perhaps including California, which has been experiencing drought conditions more often than not over the past decade and a half.
(I have always been careful to note that, scientifically, we can not say that climate
change caused a particular drought, but only that it is expected to increase the frequency, intensity, and duration of drought
in some
regions — and that such
changes are being
observed.)»