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.
Not exact matches
Assessing the
influence of individual DNA base
changes is particularly difficult
in noncoding
regions, so they instead identified bigger alterations, so - called structural variants,
in which large sequences of DNA are inverted, duplicated, or deleted.
She also thinks that though human
influence might be «greater than we realize,» this regional climate
change is probably caused by many factors, including increased irrigation
in the
region.
The exciting aspect of submergence was that they could bring
in what is known as a «quantitative trait locus» — a more genetically complex
region that
influences measurable
changes to the crop.
Within a given
region, the
change in mass due to rising or falling water reserves
influences the strength of the local gravitational attraction.
Pilot study focusing on a
region vulnerable to climate
change Although the study highlights that long term
changes in rainfall intensity are not always» man - made,» it does not necessarily mean that today's weather anomalies across the Indian Ocean rim countries and,
in particular, their frequency, are not subject to human
influence.
The author also discusses the controversial
changes in American attitudes toward the Taliban — from early support to recent bombings of Osama Bin Laden» s hideaway and other Taliban - protected terrorist bases — and how they have
influenced the stability of the
region.
Thus the
influence of aerosols must be visible mainly
in the NH and specifically
in regions downwind the sources where the largest
change in emissions has happened.
As reported
in BEA13, through collaboration with our Russian colleagues who have extensive knowledge of tree - rings
in this
region, we have learnt that the Khadyta River site has problems related to the particular site conditions that differ from other sites
in this
region, and maybe
influenced by
changing permafrost.
The argument is then that the reason trends outside the Atlantic are weak is that they aren't being
influenced by the AMO; the other explanation is that the other
regions are already over the threshold, so that the Atlantic basin is more sensitive to
changes in SSTs and atmospheric moisture than the other
regions... or the data may be poor.
The increasing severity of Australian heat waves are part of a long - term global trend towards more heat waves and hot weather
in many
regions, a trend that is very likely
influenced by human - driven climate
change.
Observational records show that anthropogenic -
influenced climate
change has already had a profound impact on global and U.S. warm season climate over the past 30 years, and there is increasing contrast between geographic
regions that are climatologically wet and dry - the hypothesis that the «wet gets wetter, dry gets drier» is seen
in a new paper by Chang et al..
This technical document aims to present a background to resource - based conflicts and how they may be
influenced by climate
change in the Asia Pacific
region.
She also thinks that though human
influence might be «greater than we realize,» this regional climate
change is probably caused by many factors, including increased irrigation
in the
region.
And because the Arctic is the fastest - warming
region on Earth, and because atmosphere and ocean
influence each other, the steady loss of sea ice each year has forced a
change in wind patterns.
In other words, under solar or anthropogenic influence the changes in mean climate values, such as the global temperature, are less important than increased duration of certain climate patterns associated say with cold conditions in some regions and warm conditions in the other regio
In other words, under solar or anthropogenic
influence the
changes in mean climate values, such as the global temperature, are less important than increased duration of certain climate patterns associated say with cold conditions in some regions and warm conditions in the other regio
in mean climate values, such as the global temperature, are less important than increased duration of certain climate patterns associated say with cold conditions
in some regions and warm conditions in the other regio
in some
regions and warm conditions
in the other regio
in the other
regions
A
change in ocean heat content can also alter patterns of ocean circulation, which can have far - reaching effects on global climate conditions, including
changes to the outcome and pattern of meteorological events such as tropical storms, and also temperatures
in the northern Atlantic
region, which are strongly
influenced by currents that may be substantially reduced with CO2 increase
in the atmosphere.
The 10 - year period ending
in 2007 witnessed fewer severe cold snaps than any other 10 - year period since record keeping began
in 1895.2 These
changes can not be explained by natural variation, and correspond very well with computer simulations that include human
influences on climate.3 Snow cover has decreased
in most
regions, especially
in the spring, and mountain snowpack has also decreased
in several
regions.4
Kroemker, D. and Mosler, H. J. (2002) Human Vulnerability — Factors
Influencing the Implementation of Prevention and Protection Measures: An Agent based Approach, Global Environmental
Change in Alpine
Regions: Recognition, Impact, Adaptation and Mitigation, Edward Elgar Publishing, Inc., 93 - 112.
Although we focus on a hypothesized CR - cloud connection, we note that it is difficult to separate
changes in the CR flux from accompanying variations
in solar irradiance and the solar wind, for which numerous causal links to climate have also been proposed, including: the
influence of UV spectral irradiance on stratospheric heating and dynamic stratosphere - troposphere links (Haigh 1996); UV irradiance and radiative damage to phytoplankton
influencing the release of volatile precursor compounds which form sulphate aerosols over ocean environments (Kniveton et al. 2003); an amplification of total solar irradiance (TSI) variations by the addition of energy
in cloud - free
regions enhancing tropospheric circulation features (Meehl et al. 2008; Roy & Haigh 2010); numerous solar - related
influences (including solar wind inputs) to the properties of the global electric circuit (GEC) and associated microphysical cloud
changes (Tinsley 2008).
Although these hydrological
changes could potentially increase soil water availability
in previously snow - covered
regions during the cool low - ET season (34), this effect would likely be outweighed by the
influence of warming temperatures (and decreased runoff) during the warm high - ET season (36, 38), as well as by the increasing occurrence of consecutive years with low precipitation and high temperature (Fig. 4A).
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 collaborative international project began
in 1993 as an effort to address how Amazonia functions as a regional entity within the larger Earth system, and how
changes in land use there might affect the
region's biological, chemical, and physical functions and
influence global climate.
The experts will be able to form an integrated evaluation based on
changes already observed, the processes known to
influence the regional climate of interest, and projections from those models that have demonstrated accuracy
in describing that
region's climate — all to a degree consistent with the kind of projection required.
Each summary begins with a brief, general overview of climate
change in BC and a short discussion of the topography, climate
influences, ecosystems and economies of the
region.
Their
influence on the atmospheric circulation is focused on the polar
regions by the Earth's magnetic field [the opposite phase of the
changes in the Arctic and the Antarctic can be explained by the phenomenon of «solar system dissymmetry» as a result of which fluctuations of solar constant occur].
Hodgson's panel, «The
Changing Landscape of ADR
in Latin America and the U.S.
Influence: A Primer for Inside and Outside Counsel,» will examine the growth of ADR
in Mexico, Brazil and Central America, as well as the factors that have negatively impacted the growth of ADR
in other parts of the
region.
Emerging Minds was overwhelmed with the support of many government and organisational representatives from around the world who shared stories about how the Australian COPMI national initiative online resources have
influenced change in their own
region and are being used to support children, families and professionals.