• Study Resource
  • Explore Categories
    • Arts & Humanities
    • Business
    • Engineering & Technology
    • Foreign Language
    • History
    • Math
    • Science
    • Social Science

    Top subcategories

    • Advanced Math
    • Algebra
    • Basic Math
    • Calculus
    • Geometry
    • Linear Algebra
    • Pre-Algebra
    • Pre-Calculus
    • Statistics And Probability
    • Trigonometry
    • other →

    Top subcategories

    • Astronomy
    • Astrophysics
    • Biology
    • Chemistry
    • Earth Science
    • Environmental Science
    • Health Science
    • Physics
    • other →

    Top subcategories

    • Anthropology
    • Law
    • Political Science
    • Psychology
    • Sociology
    • other →

    Top subcategories

    • Accounting
    • Economics
    • Finance
    • Management
    • other →

    Top subcategories

    • Aerospace Engineering
    • Bioengineering
    • Chemical Engineering
    • Civil Engineering
    • Computer Science
    • Electrical Engineering
    • Industrial Engineering
    • Mechanical Engineering
    • Web Design
    • other →

    Top subcategories

    • Architecture
    • Communications
    • English
    • Gender Studies
    • Music
    • Performing Arts
    • Philosophy
    • Religious Studies
    • Writing
    • other →

    Top subcategories

    • Ancient History
    • European History
    • US History
    • World History
    • other →

    Top subcategories

    • Croatian
    • Czech
    • Finnish
    • Greek
    • Hindi
    • Japanese
    • Korean
    • Persian
    • Swedish
    • Turkish
    • other →
 
Profile Documents Logout
Upload
Climate Change: Lessons for our Future from the Distant Past
Climate Change: Lessons for our Future from the Distant Past

... Greenhouse gases are crucial to life on earth, as they are fundamental to maintaining the planet’s temperature within limits supportive of life. There are four important greenhouse gases: water vapour (H2 O), carbon dioxide (CO2 ), nitrous oxide (N2 O), and methane (CH4 ). The last two gases have ca ...
green climate fund (gcf)
green climate fund (gcf)

... reduce greenhouse gas emissions. In addition to We have an obligation to “till and tend” the earth, as limiting future emissions, the fund will provide God told humankind in the Garden of Eden (Genesis development funding for adaptation efforts, with 2:15). God blesses the world and sees it as “good ...
ESS-ATS_543_Spring_2016
ESS-ATS_543_Spring_2016

Global and Mediterranean climate change: a short summary
Global and Mediterranean climate change: a short summary

... Since about 1750, about 374 billion metric tonnes of CO2 have been released mainly from fossil fuels combustion and cement production. Half of the total CO2 emitted from fossil fuel combustion has been registered since 1980s [33]. CO2 emissions from fossil fuel use have continued to increase during ...
Earth`s Biosphere - John Cairns, Jr.
Earth`s Biosphere - John Cairns, Jr.

1. Why does global climate change emerge?
1. Why does global climate change emerge?

... Technocrats delay and ignore the global trend of dealing with threat of climate change Logic of “valuing industrial development and ignoring risks” Lack of long term vision on global trend of developing green technology Ignore seriousness of Kyoto Protocol might lead to trade sanctions NGO protest m ...
1 - QUBES Hub
1 - QUBES Hub

... Change and Phenology Research Project” Discussion Forum. There are also additional links with resources and information on the Content page if you need more information or help with the data manipulations in Excel. The first thing you must do is introduce yourself to your group members, and state yo ...
Current and future climate of Samoa
Current and future climate of Samoa

... that take place year to year or decade to decade caused by phenomena such as the El Niño-Southern Oscillation. This variation in sea level can be seen in Figure 7 which includes the tide gauge record since 1950 and the satellite data since 1993. ...
SG-RFC-2009-doc 8-6
SG-RFC-2009-doc 8-6

... the heat and vapour exchange between the two. Trend analysis of SST provided evidence for global warming and the important climate-atmosphere feedback in the tropics that is also responsible for ENSO events. These SST observations, combined with in situ vertical temperature measurements of the ocean ...
Climate Change - European Capacity Building Initiative
Climate Change - European Capacity Building Initiative

... • Models are used to simulate the warming of the last 150 years • Their results correlate with anthropogenic + natural warming • Natural causes can’t explain what has happened. ...
South Africa
South Africa

... 2011-15 period were 0.57°C (1.03°F) above the average for the standard 1961-90 reference period. The compares with the 2006-10 period, in which temperatures were 0.51°C above average, and is consistent with a continued sustained warming trend which has been apparent in global data since the mid-1970 ...
How is Circulation in Puget Sound Projected to Change?
How is Circulation in Puget Sound Projected to Change?

... unknown  how  these  changes  will  affect  upwelling.  Changes  in  precipitation  and   streamflow  could  shift  salinity  levels  in  Puget  Sound  by  altering  the  balance  between   freshwater  inflows  and  water  entering  from  t ...
Are pattern scaling methods useful to inform about adaptation strategies?
Are pattern scaling methods useful to inform about adaptation strategies?

... transfer, for instance, if changes in hydrological cycle or atmospheric circulation are relevant [2]. The second assumption is clearly questionable for processes where changes in regional/local climate variables depend on initial state such as sea-ice and snow-albedo feedback and changes in circulat ...
Current and future climate of Vanuatu
Current and future climate of Vanuatu

... melting of glaciers and ice sheets also contributes to sea-level rise. Instruments mounted on satellites and tide gauges are used to measure sea level. Satellite data indicate the sea level has risen near Vanuatu by about 6 mm per year since 1993. This is larger than the global average of 2.8–3.6 mm ...
Effects of Climate Change on Streamflow and Water Resources
Effects of Climate Change on Streamflow and Water Resources

... Source: Payne, J.T., A.W. Wood, A.F. Hamlet, R.N. Palmer, and D.P. Lettenmaier, 2004, Mitigating the effects of climate change on the water resources of the Columbia River basin, Climatic Change, Vol. 62, Issue 1-3, 233-256 ...
PDF
PDF

... [4] The changes associated with solar variability are small, however, and the influence of solar activity on the Earth’s climate remains a controversial topic with many open questions [Lean, 1997; Foukal et al., 2006]. Although their contribution to recent warming is negligible [Lean and Rind, 2008; ...
Full text of speech by Lord Stern on environmental justice and climate change 10 September 2015, Vatican City
Full text of speech by Lord Stern on environmental justice and climate change 10 September 2015, Vatican City

Alaska Climate Research Center
Alaska Climate Research Center

... have many summaries, products, meteorological, and climatological information available. The website (http://akclimate.org/) is quite popular. From our home page, users can select any number of links: Fairbanks weather and climate, our popular webcam and on-campus ...
Danish adaptation to future climate
Danish adaptation to future climate

... Intergovernmental Panel on Climate Change (IPCC) assesses that there is a 90 per cent probability or more that the global warming we have seen over the last 50 years is due to man-made greenhouse gases. In the decades to come, Denmark will see higher temperatures and higher sea levels, just as there ...
Lesson Plan—Global Warming: How did we get here and what
Lesson Plan—Global Warming: How did we get here and what

... bring their ideas to the public. They may choose from the following suggestions or create something original: – They may visit a local elementary school or middle school and present their finding in a lesson that they will share with the class. – They may create a video that will be shown on the sch ...
28. SUMMARY AND BROADER CONTEXT
28. SUMMARY AND BROADER CONTEXT

... the role of climate change. Over the years, authors contributing to this report have also taken on the challenge of quantifying the impacts of climate change. We have increasingly emphasized this because to make attribution results informative to adaptation decisions, scientists must take on the que ...
Appendix 19 - The Work of Malcolm Roberts
Appendix 19 - The Work of Malcolm Roberts

... 8. Air movements, wind, rain, storms and hurricanes are virtually ignored. They’re too small to fit into grid systems used for each part of Earth’s surface; 9. Energy flow parameters are constants with no variability; 10. Earth has no water vapour, by far the most significant gas absorbing longwave ...
Dr Manohar Arora
Dr Manohar Arora

... The globally averaged combined land and ocean surface temperature data as calculated by a linear trend, show a warming of 0.85 [0.65 to 1.06] °C over the period 1880 to 2012. On a global scale, the ocean warming is largest near the surface, and the upper 75 m warmed by 0.11 [0.09 to 0.13] °C per dec ...
The impact of global warming on the tropical Pacific and El Niño
The impact of global warming on the tropical Pacific and El Niño

Figure 1 - Proceedings of the Royal Society B
Figure 1 - Proceedings of the Royal Society B

... adult emergence [1]. Most studies of animal phenology have exclusively examined adults, obscuring differences in exposure and sensitivity to climate across life cycles [2]. Laboratory studies examining growth and development have revealed the complex trade-offs shaping thermal responses [3], but the ...
< 1 ... 231 232 233 234 235 236 237 238 239 ... 438 >

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.
  • studyres.com © 2026
  • DMCA
  • Privacy
  • Terms
  • Report