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Causes of the northern high-latitude land surface
Causes of the northern high-latitude land surface

... the NHL land surface temperature variability. Similarly, the correlation between the AL and NHL land SAT is 0.45 for the period 1958 – 2004, only accounting for 21% of the shared variance. However, for the cooling period (during the 1960s and 1970s), the AL had a larger correlation (r = 0.65) with ...
KEY MESSAGES FOR COP 20 AND 4:17 pm
KEY MESSAGES FOR COP 20 AND 4:17 pm

... guaranteed that such funds and mechanisms effectively foster development and reach the most vulnerable communities, and not used as subsidies and risk guarantees for the private sector. Climate finance should be allocated and distributed in an equitable and non discriminatory way based on different ...
Mapping climate change research in India - e-LIS
Mapping climate change research in India - e-LIS

... changed on global scale; and warming (of 0.1°C per decade) is observed over the last 50 years is attributable to human activities. The Intergovernmental Panel on Climate Change (IPCC) projects that the global mean temperature may increase between 1.4 and 5.8 degrees Celsius by 2100. The impact would ...
West Dunbartonshire Council Climate Change Strategy `Tackling
West Dunbartonshire Council Climate Change Strategy `Tackling

... In terms of funding for actions, the Council has access to the Central Energy Efficiency Fund (CEEF) – a Government funding stream which gives the Council autonomy to fund projects which reduce energy consumption in Council property. The initial outlay is then paid back to the fund over a number of ...
Anthropocene changes in desert area
Anthropocene changes in desert area

... dust source regions [e.g., Mahowald et al., 1999]. Atmospheric carbon dioxide concentrations influence plant stomatal conductance because as CO2 diffuses into the leaf, water diffuses out. This effect is particularly pronounced under conditions of low atmospheric humidity, where stomatal control is ...
Changing monsoon patterns, snow and glacial melt, its
Changing monsoon patterns, snow and glacial melt, its

... high resolution (25 km) from 1960 to 2100, Mathison et al. (in this issue) provide another ensemble of simulations for the region, and illustrate an increase in temperature between the baseline (1970–2000) and the 2050s (2040–2070) of between 2 and 4 °C. The authors also observe an increase in the n ...
Scientific Rationale The Pliocene epoch (~ 5.33 to 2.59 Ma) is the
Scientific Rationale The Pliocene epoch (~ 5.33 to 2.59 Ma) is the

... The Pliocene epoch (~ 5.33 to 2.59 Ma) is the last sustained interval of geological time when global climate (marine and terrestrial) was significant warmer than today (Haywood et al., 2009; Naafs et al., 2010; Dowsett et al., 2012). During the late Pliocene the warm and relatively stable climate of ...
Extended Abstract
Extended Abstract

... Meteorology, University of Oklahoma, 120 David L. Boren Blvd., Rm. 5234 Norman, OK 73072-7307 ...
Slide 1
Slide 1

... Is Adaptation Occurring? A few words from the IPCC (WGII 2007) Adaptive capacity is uneven across and within societies (very high confidence). There are individuals and groups within all societies that have insufficient capacity to adapt to climate change. For example, women in subsistence farming ...
- Atmospheric Chemistry Modeling Group
- Atmospheric Chemistry Modeling Group

... Use stochastic placement of wildfires within ecosystem and ecosystem specific fuel loads. ...
How limiting factors drive agricultural adaptation to
How limiting factors drive agricultural adaptation to

... on other agronomic and socio-economic limiting factors. For example, a farmer’s debt load may have a profound effect on their ability to implement irrigation, which may help them respond to water as a limiting factor. We hope that future work can assess the interaction of these potential factors and ...
Carbon Budgets - National Assembly for Wales
Carbon Budgets - National Assembly for Wales

... GHG emissions by 80% in 2050 from 1990 levels to meet its international climate change obligations6. Part 1 of the Climate Change Act 2008 legally binds the UK to this target as well as a number of five-year carbon budgets, which ensure that regular progress is made towards the overall target. The A ...
5.6.2 Water temperature
5.6.2 Water temperature

... Species and habitat dynamics in the face of climate change are complex and have many aspects. Increased temperatures and increased CO2 concentrations will have an effect on different processes such as photosynthesis, respiration and decomposition and generally speed up these processes. Climate induc ...
M B V C
M B V C

... SAJEMS NS 17 (2014) No 5:639-652 ...
Projected climate-induced faunal change in the Western Hemisphere
Projected climate-induced faunal change in the Western Hemisphere

... the 30 climate-change projections to estimate potential faunal changes for each of the 15 323 50-km grid cells in the Western Hemisphere. As climate changes, species will differ in their ability to track the change and to move into newly created suitable habitat. We calculated potential faunal chang ...
climate impacts and adaptation unit
climate impacts and adaptation unit

... Decision-makers may therefore be reluctant to allocate staff time and financial resources to analysing and adapting to the physical effects of climate change. Hence, a critical precursor to developing an adaptation strategy for your organisation is to convince the “powers that be” of the case to imp ...
Climate Solutions based on advanced scienti c discoveries of Allatra
Climate Solutions based on advanced scienti c discoveries of Allatra

... Recently, at the end of the 20th century, scientists put forward various hypotheses and theories about gradual climate change. But in practice everything turned out to be somewhat different. A thorough analysis of the growing number of natural disasters and extreme weather events around the world, i ...
Terrestrial biogeochemical feedbacks in the climate system
Terrestrial biogeochemical feedbacks in the climate system

... standard deviations (white). For calculations, adopted from ref. 6, and data sources see Supplementary Information. Totals include top-end estimates, without and with (black rectangle) C–N interactions. Estimates are based on a number of assumptions that had to be made and clearly point to the need ...
How limiting factors drive agricultural adaptation to climate change.
How limiting factors drive agricultural adaptation to climate change.

... on other agronomic and socio-economic limiting factors. For example, a farmer’s debt load may have a profound effect on their ability to implement irrigation, which may help them respond to water as a limiting factor. We hope that future work can assess the interaction of these potential factors and ...
Government of Nepal Ministry of Population and Environment
Government of Nepal Ministry of Population and Environment

... years. In the case of hydropower, the model projected lower dry season flows and thus lower energy availability. The additional energy generation capacity needed to meet future demand under this scenario, due to climate change, was estimated at 2800 MW by 2050 with an increase in costs of USD 2.6 bi ...
climate impacts and adaptation unit
climate impacts and adaptation unit

... Decision-makers may therefore be reluctant to allocate staff time and financial resources to analysing and adapting to the physical effects of climate change. Hence, a critical precursor to developing an adaptation strategy for your organisation is to convince the “powers that be” of the case to imp ...
Small Business Sector - American Sustainable Business Council
Small Business Sector - American Sustainable Business Council

... is currently not on a path to meet the International Panel on Climate Change’s (IPCC) mitigation target of a 50 percent reduction in global greenhouse gases by 2050, a goal set to avoid the world’s average temperature from rising in excess of 2 degrees Celsius, strategies to prepare for a warming cl ...
Climate Actions in EU and Globally
Climate Actions in EU and Globally

... – The capped sector uses all of international offsets allowed in all years of the policy (1.25 billion tCO2e offsetting 1 billion tCO2e of capped sector emissions annually) – International offsets produced from REDD, afforestation, and forest management – The 1 billion tCO2e annual limit on domestic ...
Silencing Science
Silencing Science

... attendee at the Kochs’ secret major-donor summits.26 Its staff is also made up of past employees of Koch-funded groups such as the American Legislative Exchange Council (ALEC) and the Mercatus Center. Charles Koch was involved in founding the Institute for Energy Research, AEA’s charitable arm, whic ...
Now more than ever: The need for more societally
Now more than ever: The need for more societally

... 2006; Walker, Holling, Carpenter, & Kinzig, 2004). To the extent systems can be resilient over time while providing equitable access to life support and the basis for livelihood and economic activity, they may be considered sustainable (e.g., Eakin & Webhe, 2009; Perrings, 2006; for a detailed revie ...
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Climate change and agriculture



Climate change and agriculture are interrelated processes, both of which take place on a global scale. Climate change affects agriculture in a number of ways, including through changes in average temperatures, rainfall, and climate extremes (e.g., heat waves); changes in pests and diseases; changes in atmospheric carbon dioxide and ground-level ozone concentrations; changes in the nutritional quality of some foods; and changes in sea level.Climate change is already affecting agriculture, with effects unevenly distributed across the world. Future climate change will likely negatively affect crop production in low latitude countries, while effects in northern latitudes may be positive or negative. Climate change will probably increase the risk of food insecurity for some vulnerable groups, such as the poor.Agriculture contributes to climate change by (1) anthropogenic emissions of greenhouse gases (GHGs), and (2) by the conversion of non-agricultural land (e.g., forests) into agricultural land. Agriculture, forestry and land-use change contributed around 20 to 25% to global annual emissions in 2010.There are range of policies that can reduce the risk of negative climate change impacts on agriculture, and to reduce GHG emissions from the agriculture sector.
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