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Migration and Climate Change - Development Research Centre on
Migration and Climate Change - Development Research Centre on

... secuted for reasons of race, religion, nationality, membership of a particular social group, or political opinion, is outside the country of his nationality, and is unable to or, owing to such fear, is unwilling to avail himself of the protection of that country”.14 There are other problems with us ...
Climate Change in Kiana, Alaska - Alaska Native Tribal Health
Climate Change in Kiana, Alaska - Alaska Native Tribal Health

... activity (IPCC, 2008). In Kiana, the rate of climate change can be measured in months, days, or even hours. Residents traveling the river encounter sections of collapsed riverbank that were intact only hours before. In every season of the year, the air temperature is warmer than it was in the past. ...
બાળ વિજ્ઞાન કોગ્રેસ ૨૦૧૫ વિષય: hvimin an[ aibi[hvi
બાળ વિજ્ઞાન કોગ્રેસ ૨૦૧૫ વિષય: hvimin an[ aibi[hvi

... s)F[s)F&> j mYiL&> ni[>Fi[. TiETl T*>k&> hi[v&> ji[Ea[ an[ b[ Y) vFir[ l)T) n Yiy. aºy pi[ATs< {1}p\i[j[±T TiETl {2}j*Yni s¿yi[ni nim {3}h[t&ai[ {4}(vAtirni[ n±Si[ {5}p¹F(t {6}p(rNimi[ {7}tirNi[ {8}smAyini uk[ln[ smivti rcvi. j[mi> (vAtirni[ n±Si[ m*kvi[ j$r) C[ k[ k[m t[ p\i[j[±T upr aiFi(rt C[. pi ...
Quantitative Assessment of Climate Carrying Capacity for Cities: A
Quantitative Assessment of Climate Carrying Capacity for Cities: A

... Recent research on carrying capacity has mostly focused on ecological carrying capacity, water resources carrying capacity, land carrying capacity, population carrying capacity, and environmental carrying capacity. However, such research has often treated the climate condition as a stable background ...
Constructing Sea-Level Scenarios for Impact and Adaptation
Constructing Sea-Level Scenarios for Impact and Adaptation

... Figure 2: Summary of a methodology commonly applied for developing sea-level scenarios for impact assessment and adaptation planning. MSL – mean sea level; ESL – extreme sea level. ........................ 5 Figure 3: The estimated budget of the components of global mean sea level change (A), their ...
Climate Change Adaptation Position Paper
Climate Change Adaptation Position Paper

... Adapting to future climate change is an important concept both on a national and global scale. Both ecosystems and society will need to adapt to the new climatic conditions that global warming will inevitably bring. Society will face significant challenges in adapting to global warming. This is part ...
Climate Change: ImplIcatIons and strategIes for the luxury fashIon
Climate Change: ImplIcatIons and strategIes for the luxury fashIon

... to the impact of climate change: input, physical, market, stakeholder, and regulatory.5 In light of these risks and the fact that the importance of different risks will vary over time and over geographies, it is imperative that companies take a deep look at their supply chains and operations to unde ...
Small global-mean cooling due to volcanic radiative forcing
Small global-mean cooling due to volcanic radiative forcing

... Received: 18 September 2015 / Accepted: 19 February 2016 © The Author(s) 2016. This article is published with open access at Springerlink.com ...
Agreeing to disagree: Uncertainty management in assessing climate
Agreeing to disagree: Uncertainty management in assessing climate

... Groups, and do not exclude that other dimensions could also be considered. The division between the objective and the subjective views of probabilities is the oldest. Objective views of probabilities include the classical approach (probability is the proportion of favorable cases over total cases), ...
Mexico - Met Office
Mexico - Met Office

... climate has changed and will continue to change in future in response to human activities. Across the world, this is already being felt as changes to the local weather that people experience every day. Our ability to provide useful information to help everyone understand how their environment has ch ...
PDF
PDF

... comprehensively assess transportation vulnerabilities and prepare for the unavoidable impacts of climate change. Recent studies indicate that climate change planning efforts conducted by governments thus far have overwhelmingly focused on mitigation strategies to reduce greenhouse gas (GHG) emission ...


Effects of Seasonal Weather on Breeding Phenology
Effects of Seasonal Weather on Breeding Phenology

... breeding attempts in a breeding season (e.g., [12]), and annual productivity is generally lower in high-elevation systems [13, 14, 15]. Reduced breeding opportunities may cause greater variability in annual fecundity as stochastic events such as extreme spring weather delaying breeding should have l ...
Document
Document

... The eastern Arabian Sea hosts one of the most intense Oxygen Minimum Zones (OMZ) in the world. Changes in monsoon airflow and subsurface circulation drive OMZ variations in the region. Sediments from the region hosting evidence of past OMZ change have rarely been studied. Hence, retrieving high-qual ...
Meeting the Challenge of Climate Change
Meeting the Challenge of Climate Change

... contributing to the rise in sea levels. In the Arctic, in particular, over the last 100 years, temperatures have been increasing at almost twice the global average rate. For most of Canada, this translates into temperature increases both on a seasonal basis, with winters warming more than summers, a ...
An Integrated Assessment of Changes in the Thermohaline Circulation
An Integrated Assessment of Changes in the Thermohaline Circulation

... the elicitation among leading ocean experts presented later in this paper reveals widely differing views about the probability of a shutdown being triggered this century, with some estimates even exceeding the 50% level for scenarios with high global temperature rise. Narrowing down this uncertainty ...
A Unified Sea Level Rise Projection for Southeast Florida April 2011
A Unified Sea Level Rise Projection for Southeast Florida April 2011

... release of United Nations Intergovernmental Panel on Climate Change Fifth Assessment Report. The scientific evidence strongly supports that sea level is rising and, beyond 2060, will continue to rise even if mitigation efforts to reduce greenhouse gas (GHG) emissions are successful at stabilizing or ...
A Unified Sea Level Rise Projection for Southeast Florida April 2011
A Unified Sea Level Rise Projection for Southeast Florida April 2011

... release of United Nations Intergovernmental Panel on Climate Change Fifth Assessment Report. The scientific evidence strongly supports that sea level is rising and, beyond 2060, will continue to rise even if mitigation efforts to reduce greenhouse gas (GHG) emissions are successful at stabilizing or ...
Climate change in the Norwegian Arctic – Consequences for life in
Climate change in the Norwegian Arctic – Consequences for life in

... expertise concerning climate conditions in the Norwegian part of the Arctic, and to identify areas in which knowledge is incomplete. Within the framework of NorACIA, focus is on communication, advice to the government on management issues and compilation about climate change in the Norwegian Arctic. ...
a post-IPCC AR4 update on sea- level rise
a post-IPCC AR4 update on sea- level rise

... contributions to recent sea-level rise • Observations since 1961 show that the oceans have warmed as the result of absorbing more than 80% of the heat added to the climate system largely because of the enhanced greenhouse effect. The warming has caused the oceans to expand, contributing to sea-leve ...
ENSO Effects on Land Surface-Biosphere
ENSO Effects on Land Surface-Biosphere

... Atmospheric responses to ENSO events lead to change in land surface parameters. Jin and Dickinson (2010) suggest that there are two key mechanisms for changes in land surface parameters: large-scale dynamics and local effects. Large-scale dynamics are the physical processes over large-scale areas th ...
Climate Change, Migration, and Displacement | Greenpeace
Climate Change, Migration, and Displacement | Greenpeace

Phenology, biomass and community composition  changes in European shrublands submitted to
Phenology, biomass and community composition changes in European shrublands submitted to

View PDF - CiteSeerX
View PDF - CiteSeerX

... 1998); however, they may be able to move more quickly (Clark, 1998; Clark et al., 1998). Even the relatively rapid migration rates of the past have proven difficult to explain; for example, it appears necessary to invoke infrequent longdistance dispersal events that are inherently difficult to quant ...
Climate: Observations, projections and impacts
Climate: Observations, projections and impacts

... climate has changed and will continue to change in future in response to human activities. Across the world, this is already being felt as changes to the local weather that people experience every day. Our ability to provide useful information to help everyone understand how their environment has ch ...
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Global warming hiatus



A global warming hiatus, also sometimes referred to as a global warming pause or a global warming slowdown, is a period of relatively little change in globally averaged surface temperatures. In the current episode of global warming many such periods are evident in the surface temperature record, along with robust evidence of the long term warming trend.The exceptionally warm El Niño year of 1998 was an outlier from the continuing temperature trend, and so gave the appearance of a hiatus: by January 2006 assertions had been made that this showed that global warming had stopped. A 2009 study showed that decades without warming were not exceptional, and in 2011 a study showed that if allowances were made for known variability, the rising temperature trend continued unabated. There was increased public interest in 2013 in the run-up to publication of the IPCC Fifth Assessment Report, and despite concerns that a 15-year period was too short to determine a meaningful trend, the IPCC included a section on a hiatus, which it defined as a much smaller increasing linear trend over the 15 years from 1998 to 2012, than over the 60 years from 1951 to 2012. Various studies examined possible causes of the short term slowdown. Even though the overall climate system had continued to accumulate energy due to Earth's positive energy budget, the available temperature readings at the earth's surface indicated slower rates of increase in surface warming than in the prior decade. Since measurements at the top of the atmosphere show that Earth is receiving more energy than it is radiating back into space, the retained energy should be producing warming in at least one of the five parts of Earth's climate system.A July 2015 paper on the updated NOAA dataset cast doubt on the existence of this supposed hiatus, and found no indication of a slowdown. This analysis incorporated the latest corrections for known biases in ocean temperature measurements, and new land temperature data. Scientists working on other datasets welcomed this study, though the view was expressed that the short term warming trend had been slower than in previous periods of the same length.
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