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gcc_press re collapse_all_1_001
gcc_press re collapse_all_1_001

... Detroit News, March 3,2000, “Detroit could see red, feel blue over not being green enough,” by Jon Pepper. Global Warming Today, March 2,2000, “Texaco Announces Decision to Leave GCC.” WashinPton Post, March 2,2000, “Texaco, the third-largest U.S. oil company, said it’s dropping out of the Global Cl ...
Extreme Weather Events and Disaster Preparedness
Extreme Weather Events and Disaster Preparedness

... part of the country. The dwindling water resources of the sub-region which has drastically reduced opportunities for sustainable agriculture is a contributing factor to the current conflicts and high degree of insecurity being witnessed in the area.  Mount Kilimanjaro Glaciers: The gradual yet dram ...
this publication
this publication

... estimated  at  a  reduction  of  0.1  units  of  pH  since  pre-­‐industrial  levels  (Meehl  et  al.,  2007  in  IPCC   AR4).  Note  that  a  lower  pH  value  indicates  higher  acidity.  Reduced  reef  calcification  due  to   acid ...
Use of models in detection and attribution of climate change
Use of models in detection and attribution of climate change

... recent greenhouse gas levels far exceed previous levels (‘The combined radiative forcing due to increases in carbon dioxide, methane, and nitrous oxide is +2.30 [+2.07 to +2.53] W m−2 , and its rate of increase during the industrial era is very likely to have been unprecedented in more than 10,000 y ...
Telling the Weather Story - Institute for Catastrophic Loss Reduction
Telling the Weather Story - Institute for Catastrophic Loss Reduction

... 0.13°C per decade, and for the last 25 years of the record, mean temperature rose by 0.18°C per decade. Note also that the trend is much more consistent when averaged over a few years, and the most recent rate of warming approaches being three times higher than over the century as a whole. Based on ...
Stream 1.2 Oceans and marine ice in the Southern Hemisphere
Stream 1.2 Oceans and marine ice in the Southern Hemisphere

... To understand the extent of large-scale physical, biological and biogeochemical change occurring in the Southern Ocean and marine ice environment (including ice shelves, sea ice and icebergs), and to attribute the cause(s) to anthropogenic emissions or natural variations for inclusion in IPCC models ...
PDF
PDF

... potential for trade to play this buffering role is often hampered by restrictive trade practices. When individual countries insulate their domestic markets from developments in other regions they jeopardize the ability of world markets to lower global costs of climatic change. The value of this spat ...
- Wiley Online Library
- Wiley Online Library

The Carbon Dioxide Greenhouse Effect
The Carbon Dioxide Greenhouse Effect

... Tyndall set out to find whether there was in fact any gas in the atmosphere that could trap heat rays. In 1859, his careful laboratory work identified several gases that did just that. The most important was simple water vapor (H2O). Also effective was carbon dioxide (CO2), although in the atmospher ...
Visual Salience in Climate Change Imagery is in the Eye of the
Visual Salience in Climate Change Imagery is in the Eye of the

... Visual Salience in Climate Change Imagery is in the Eye of the Beholder Complex phenomena like climate change are often communicated visually. In this paper, we investigated the effectiveness of common visuals used to convey key messages about climate change. We also present a new methodology for a ...
Chapter 6 Climate Science and Politics in the United States
Chapter 6 Climate Science and Politics in the United States

... underscored climate change concerns (Study of Critical Environmental Problems 1970; Study of Man's Impact on Climate 1971). The entrepreneurial professor Caroll Wilson of MIT’s Sloan School of Management, a long-time government science advisor and a member of the Club of Rome, organized both studies ...
Why tropical forest lizards are vulnerable to climate warming
Why tropical forest lizards are vulnerable to climate warming

... (thermoconformers that live in forests) are active at low body temperature and are intolerant of warm temperatures. Focal species analyses show that some tropical forest lizards were already experiencing stressful body temperatures in summer when studied several decades ago. Simulations suggest that ...
The Climate System: an Overview
The Climate System: an Overview

... to season, year to year, decade to decade or on much longer time-scales, such as the Ice Ages. Statistically significant variations of the mean state of the climate or of its variability, typically persisting for decades or longer, are referred to as “climate change”. The Glossary gives definitions ...
Why Have Climate Negotiations Proved So Disappointing?
Why Have Climate Negotiations Proved So Disappointing?

... 2007). Moreover, we don’t know the quantity of global emissions (expressed, perhaps, as a cumulative sum) needed to meet any particular concentration target, due to uncertainty in the carbon cycle. For example, there is uncertainty about how much of the CO2 emitted will be taken up by soils and the ...
The Changing Himalayas - India Environment Portal
The Changing Himalayas - India Environment Portal

... Summary: The greater Himalayan region “the roof of the world” – contains the most extensive and rugged high altitude areas on Earth, and the largest areas covered by glaciers and permafrost outside the polar regions. The water resources from this area drain through ten of the largest rivers in Asia, ...
Weather GuideBook Rubric
Weather GuideBook Rubric

... composition of the atmosphere and the quantities (percentage) of each gas. Explain how composition and temperature are related. Layers of the atmosphere: Illustration (Graph the relationship between altitude, air pressure, and temperature). Describe each layer and include important facts about each ...
Toward Integrated Historical Climate Research
Toward Integrated Historical Climate Research

... and modelling, and a lack of engagement with cultural climate history.2 Determining both the likely future climates and how different communities might be affected by and respond to climate change, however, has become an issue of global and political importance. Establishing a multidisciplinary dia ...
Stream 1.2 Oceans and marine ice in the Southern Hemisphere
Stream 1.2 Oceans and marine ice in the Southern Hemisphere

... To understand the extent of large-scale physical, biological and biogeochemical change occurring in the Southern Ocean and marine ice environment (including ice shelves, sea ice and icebergs), and to attribute the cause(s) to anthropogenic emissions or natural variations for inclusion in IPCC models ...
Philosophy of Climate Science Part I: Observing
Philosophy of Climate Science Part I: Observing

... These various ways of obtaining data raise a host of philosophical problems. First of all, the use of instruments to obtain data, e.g., of thermometers to measure the temperature, raises the question of theory-ladenness of observation. This is a classical topic that has been extensively discussed in ...
Climate Scientists and the Consensus on Climate Change
Climate Scientists and the Consensus on Climate Change

... proportion (37%) anticipating ‘some positive effects’ for the country in which they lived again was lower than the proportion (45%) that anticipated ‘positive effects’ for ‘other parts of the world’. A similar question about detrimental effects was not asked (2008, figs. 27a, 27b). What do climate s ...
Climate change impacts on crop production in Iran`s Zayandeh
Climate change impacts on crop production in Iran`s Zayandeh

... and volume of water used (m 3). Higher temperatures can generally increase the irrigation water requirement. While increased irrigation can result in higher crop production even under higher temperatures, generally lower crop production is expected with global warming due to the limited water supply ...
analysis.
analysis.

... Ward turned to an analogy when suggesting how writers should handle individual events within the context of climate change. Imagine teams playing a pair of basketball games — matches identical in all respects save one: The floor on the first court is six inches higher than the second. Will the game ...
A consistent poleward shift of the storm tracks in simulations of 21st
A consistent poleward shift of the storm tracks in simulations of 21st

... [9] In this paper, we represent the storm tracks using eddy kinetic energy (EKE) that has been filtered to retain variability on synoptic time scales of 2 – 8 days. We begin by examining the consensus among the models as represented by the 15-member multi-model ensemble. The multimodel mean 2081 –21 ...
Syllabus - The Bodanyi Project
Syllabus - The Bodanyi Project

... define global climate change as a policy problem. We will learn about the basics of carbon cycle, assessment tools available to model global climate change and its impacts at the global as well as regional levels. Lastly, we will examine alternative ways governments have used to frame global climate ...
The Household Production Function Approach to Valuing Climate
The Household Production Function Approach to Valuing Climate

... Summarising the literature, some studies employ international data but most use data from a single country. 7 Particularly in cross-country studies data are frequently aggregated over large, climatically diverse regions. Most studies include temperature and precipitation but far fewer include other ...
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Instrumental temperature record



The instrumental temperature record shows fluctuations of the temperature of earth's climate system. Initially the instrumental temperature record only documented land and sea surface temperature, but in recent decades instruments have also begun recording ocean temperature. Data is collected from thousands of meteorological stations around the globe and through satellite observations. The longest-running temperature record is the Central England temperature data series, that starts in 1659. The longest-running quasi-global record starts in 1850.
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