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L31-Impacts - Boston University
L31-Impacts - Boston University

... Apr-23 & 25-07 (10 of 16) ...
JPI Climate
JPI Climate

... 1. JPI Climate Workshop Towards Open Climate Knowledge - Potentials and Weaknesses of the Access to Knowledge Approach on Climate Services: Jan. 13-14, 2015, Vienna 2. JPI Climate Workshop Integrated socio-economic policy and response analysis, 21-22 ...
Global marine analysis suggests food chain collapse
Global marine analysis suggests food chain collapse

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PDF

... individual regions, there is substantial variation across models in predicted effects, reflecting differences in climate change predictions Save web pages as PDF manually or automatically with PDFmyURL ...
cop21 and the paris agreement
cop21 and the paris agreement

... tackle human-induced climate change. At COP17 in Durban four years ago, the deadline of 2015 was set for agreement of a new universal protocol to limit greenhouse gas (GHG) emissions, with implementation envisaged from 2020 onwards. After two decades of negotiations, COP21 was therefore expected to ...
Climate impacts threatening Japan today and tomorrow
Climate impacts threatening Japan today and tomorrow

... increased for Japan. This type of change could translate into more unpredictable rainfall patterns, which would make planning for agriculture and water resource management more difficult. In some areas of Japan, significant decreasing trends in annual mean rainfall have been observed (Cruz et al., 2 ...
JPI Climate, H2020, & Climate Change Frank McGovern October 2
JPI Climate, H2020, & Climate Change Frank McGovern October 2

...  The global goal is to maintain the planet within 2°C warming  We have already emitted more than 50% of the allowable cumulative GHG emissions for this;  At current levels, this limit will be reached before 2050.  Impacts are evident everywhere and will increase e.g. sea-level rise.  Adaptation ...
Cenozoic Cooling Research Paper
Cenozoic Cooling Research Paper

Expert Judgment for Climate Change Adaptation
Expert Judgment for Climate Change Adaptation

... Our main focus here is a third path to the same conclusion: making explicit the implications of the most recent report from the IPCC. Each climate projection project is based on a set of methodological assumptions, and these can be subjected to scrutiny. Frigg, Smith, and Stainforth (2013, 2015) ana ...
LCCARL231_en.pdf
LCCARL231_en.pdf

... US Congressional Budget Office, 2003 US Congressional Budget Office, 2003 ...
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PDF

Elemental Geosystems, 5e (Christopherson)
Elemental Geosystems, 5e (Christopherson)

... B) They show the lack of scientific agreement about whether the climate is changing. C) They state that glacial ice is melting worldwide, and river and lake ice is melting sooner in the spring. D) They include new and stronger evidence that most of global warming is human caused. E) The Third Assess ...
Our Climate Options Have Shrunk
Our Climate Options Have Shrunk

... • Oxford University's Prof John Broome, a IPCC WG3 lead author: "At our IPCC meeting, they treated the SPM (Summary for Policymakers) as though it were a legal document rather than a scientific report. To achieve consensus, the text of the SPM was made vaguer in many places, and its content diluted ...
X - The Heartland Institute`s International Conferences on Climate
X - The Heartland Institute`s International Conferences on Climate

... changes over the past century, but the best match with observations is obtained in (c) when both natural and anthropogenic factors are included. These results show that the forcings included are sufficient to explain the observed changes, but do not exclude the possibility that other forcings may al ...
Research Project Final Report
Research Project Final Report

... with any other significant events and options for new work. The purpose of the project can be simply summarised as coordination and drafting of the climate change contribution for the OSPAR QSR in 2010. The OSPAR Quality Status Report 2010 will report on the development of the quality status of the ...
Climatic warming strengthens a positive feedback between alpine
Climatic warming strengthens a positive feedback between alpine

... In alpine and arctic ecosystems, warming experiments and long-term monitoring have documented significant increases in the growth and cover of woody species (Sturm et al., 2001; Walker et al., 2006; Myers-Smith et al., 2011). The frequency and extent of wildfires in these environments have also incr ...
Tropical Belt WG
Tropical Belt WG

... The tropics are a fundamental climate zone on Earth, characterized by a band of deep convective storms along the Equator, known as the Intertropical Convergence Zone (ITCZ), and bounded by arid regions in the subtropics of each hemisphere, such as the African and Australian deserts. Together, th ...
The benefits of recent warming for maize production in high latitude
The benefits of recent warming for maize production in high latitude

... For these northern regions, temperatures are not currently above the optimum level for maximum photosynthesis rates for many crops, so that warming could increase crop growth in these regions. Meanwhile, the gain in available growing degree days between frosts (GDDavailable) implies opportunities fo ...
PMIP
PMIP

... models can be very useful to investigate the physical mechanisms of climate change. They can be used for example to test the sensitivity of the climate system to supposed forcing of past climates such as variations in solar radiation, ice sheet extent or CO2. ...
Grand Minimum of the Total Solar Irradiance Leads to
Grand Minimum of the Total Solar Irradiance Leads to

... The climatic system is affected by a quasi-bicentennial cyclic external action connected with corresponding variations of the TSI. Significant cyclic climate changes are a forced response of the climatic system to these external actions. The basic features of climate variations are connected, in par ...
East Africa
East Africa

... from several climate models through objective weighting is ongoing (e.g., Giorgi and Mearns 2002, 2003; Tebaldi et al. 2004, 2005). Using the Bayes theorem and making certain assumptions, it is possible to objectively assign weights to different climate models leading to a probability distribution o ...
Annual and seasonal mean temperatures in Finland during the
Annual and seasonal mean temperatures in Finland during the

... the northern part of the country, Lapland, started relatively late compared to the other parts of the country: Copyright  2009 Royal Meteorological Society ...
ICLEI Milestone 2 Report Climate Changes and Impacts for the City
ICLEI Milestone 2 Report Climate Changes and Impacts for the City

... Historical trends at local stations The high natural variation in precipitation makes it more difficult to determine long term trends, especially for climate stations with shorter records. Most of the region experienced little change in annual precipitation, with small increases in the west, includi ...
The effect of development on the climate sensitivity of agriculture
The effect of development on the climate sensitivity of agriculture

... outcome of warming in both the United States and India. In order to appreciate the data upon which the analysis rests, we present the range of climates observed for each country in table 3. The temperature range for each country is large compared to temperature changes predicted by warming. The diff ...
Climate Change
Climate Change

... equations are applied to see how much air/heat flows between each pair of cells – This is repeated all around the Earth – The models have improved by making the cells smaller – They are now about 110 km square by 1 km high ...
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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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