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Twentieth-Century Global-Mean Sea Level Rise: Is the Whole
Twentieth-Century Global-Mean Sea Level Rise: Is the Whole

... time series with a constant vertical offset to make them join at 2000, and they match well at 2000 regarding rate of rise. At the time of writing, results are becoming available from CMIP5 AOGCMs, which extend to 2005. We have not used these because they will require detailed analysis, such as the C ...
Why Physical Geography matters - School of Geography and the
Why Physical Geography matters - School of Geography and the

... 8 reasons why desert dust is very important and why we need to know more about it A critical part of the linked land‐sea‐air global system ...
Author`s personal copy
Author`s personal copy

... models assessed in the IPCC AR4’’—with summer sea ice now well below the IPCC worst case scenario (Allison et al., 2009, pp. 29–30). Summer minimum sea ice was higher in subsequent years, but still fell near or below the long-term observed downward trend (which, as just noted, declines faster than t ...
Climate and Vegetation Phenology
Climate and Vegetation Phenology

... no trend in snow-water equivalent from 1939 through 2010, and snowwater equivalent at Lake Camp trended upward at a rate of 34 millimeters per century from 1936 through 2010. The annual peak snow depth at the moderately high elevation of the Lake Yellowstone climate station (2,368 meters elevation) ...
Major Climate Feedback Processes Water Vapor Feedback Snow
Major Climate Feedback Processes Water Vapor Feedback Snow

...  The saturated mixing ratio is a function of air temperature: the warmer the temperature the larger the saturated mixing ration.  a warmer atmosphere can carry more water vapor  stronger greenhouse effect  amplify the initial warming  one of the most powerful positive feedback ...
June 2013 ISSN 2070-4593
June 2013 ISSN 2070-4593

... be agreement on the policy priorities and key themes to be addressed in the Draft Policy obtained through an open, transparent and inclusive consultative process. Further a Draft CARICOM Policy and Action Programme in relation to the environment and natural resources management would have been devel ...
Full text
Full text

... supporting development finally aim to promote potentialities and expand opportunities for people. In developing countries, millions of the poorest of the world is facing climate change threats. Drought, floods occur even more serious. Increasing environmental pressures are hampering the efforts of t ...
The influence of dynamic vegetation on the present
The influence of dynamic vegetation on the present

... (GCMs) remains one of the central problems in providing accurate projections of climate change for the next 50 to 100 yr (Randall et al., 2007). Although great advances in global modelling have been made in recent decades (Solomon et al., 2007), there are still large uncertainties in many processes ...
Present and future responses of growing degree days for
Present and future responses of growing degree days for

... et al., 2017b) or decreased land precipitation (Paparrizos et al., 2016a), even the smallest diminution of water use can act towards the preservation and the sustainable development of the water resources, especially in areas where water is essential for agriculture. Finally, potential future increa ...
The Urban Physical Environment: Temperature and Urban Heat
The Urban Physical Environment: Temperature and Urban Heat

... slow laminar flow horizontal to the Earth’s surface and remains in a shallow layer, 20 to 300 m thick, even as air in the free atmospheric above the boundary layer may be moving at a much higher speed. During the day, the air at the bottom of the boundary layer becomes turbulent because of surface h ...
Climatic Impact of Volcanic Emissions
Climatic Impact of Volcanic Emissions

... chemistry [Tabazadeh and Turco, 1993]? Does the injection of water vapor from the volcanic input plus that entrained from the atmosphere, especially in a moist, tropical environment, provide an important source of stratospheric water vapor, or is the amount negligible? Would subsequent heating of th ...
Samoa
Samoa

... Climate Risk Profile (CRP). Young. W.: 2007 best estimates of long term, systematic changes in the average climate for Samoa indicate that by 2050 sea level is likely to have increased by 36 cm; rainfall shall increase by 1.2%; extreme wind gusts by 7%, and maximum temperatures by 0.7˚ C. However, t ...
The Influence of Climate Variability and Change on the Science and
The Influence of Climate Variability and Change on the Science and

... unusually cool and dry weather in the Pacific Northwest, with reversed expression during La Niña events. Multidecadal (twenty-year to sixty-year) periodicities in the climate system have also been identified but remain poorly understood mechanistically in part because the instrumental record capture ...
Developments of the IOC science programme and
Developments of the IOC science programme and

... RADIALES, ESTOC, and the Western Channel Observatory, have helped resolve the biogeochemical variability in the ocean. The information obtained via their measurements play a critical role in elucidating current and future changes of marine ecosystem driven both by anthropogenic and natural causes. G ...
Natural hazards and farmers experience of climate change on highly
Natural hazards and farmers experience of climate change on highly

... is changing the seasonal patterns are expected to become more extreme. This influences how the land can be used, and has a strong impact on the farmers who depend on their land for economic income and food security. This report has two aims. The first is to identify the farmer’s experiences of clima ...
Climate Stabilization at 2°C and Net Zero Carbon Emissions
Climate Stabilization at 2°C and Net Zero Carbon Emissions

... 9.5 in IPCC 2013). Historical (1861–2005) simulations with MESM showed that the use of a lower value of CS (e.g., 1.5°C) would require the use of a very low rate for oceanic heat uptake to produce surface warming consistent with available observations. This, however, would result in a very substanti ...
CLIMATE CHANGE IMPACTS IN NEW ZEALAND: A CROSS
CLIMATE CHANGE IMPACTS IN NEW ZEALAND: A CROSS

... The key changes in Step 1 above were the climate projections from NIWA, demographics, social variables, and wildcard variables. In summary, for the social scenarios we assumed an overall growth in the New Zealand population up to over five million people by the 2080s with larger Maori, Pacific Islan ...
PDF
PDF

... Rather than using precipitation variables, I rely directly on measures of water content in the soil. While disaggregated weather data can be obtained with relative ease, this is not the case for soil moisture. Detailed soil moisture measurements are typically confined to experimental fields in some ...
Emerging markets and climate change: Mexican standoff or low-carbon race?: Working Paper 46 (489 kB) (opens in new window)
Emerging markets and climate change: Mexican standoff or low-carbon race?: Working Paper 46 (489 kB) (opens in new window)

... extremely significant contribution to 21st century climate change, and this is easily neglected in a two-agent model. Yet it turns out that growth pathways in emerging markets are crucial to our ability to avoid dangerous anthropogenic climate change, and this has implications for the normative dime ...
How Climate Science Became a Victim of the Cold War
How Climate Science Became a Victim of the Cold War

... given the steady increase in atmospheric CO2 (and other greenhouse gases) we may reasonably expect to see effects on Earth’s climate. And we have. Instrumental measurements reveal an increased average global surface temperature of approximately 0.8o C since the 1860s, when sustained systematic recor ...
LEARN ABOUT… Climate change and ozone depletion
LEARN ABOUT… Climate change and ozone depletion

... Total column ozone annual mean anomalies for different data sets. Anomalies are with respect to the 1998 to 2008 mean of each individual data set. Coloured lines give observed results for the data sets. Grey line and grey range give multi-model mean and ±2 standard deviation range of annual mean ano ...
Where Is the North Pole? An Election
Where Is the North Pole? An Election

... Where Is the North Pole? An Election-Year Survey on Global Change Lawrence C. Hamilton ...
PDF
PDF

... citizens cannot be satisfied without significantly increasing global energy use, and CO2 emissions. Therefore, the author asserts that climate engineering and adaptation are preferable to mitigation, particularly since the science is less than adequate for making firm statements about the Earth’s fu ...
Lesson: Concerning Climate- Weather Matters
Lesson: Concerning Climate- Weather Matters

... area during different parts of the year, such as seasons and average temperature. When a change occurs in climate, it can affect the average for the area. For example, a global average temperature rise as little as 1°F can lead to severe weather events like storms or droughts because heat is a drivi ...
Turn Down The heaT: why a 4°C warmer worlD musT Be avoiDeD
Turn Down The heaT: why a 4°C warmer worlD musT Be avoiDeD

... And most importantly, a 4°C world is so different from the current one that it comes with high uncertainty and new risks that threaten our ability to anticipate and plan for future adaptation needs. The lack of action on climate change not only risks putting prosperity out of reach of millions of pe ...
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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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