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Present weather and Climate: evolving Conditions
Present weather and Climate: evolving Conditions

... The linear warming trend continued in the first decade of the twenty-first century, the warmest over the region during the 110-year period of record (see Table 5.1). Increases have been more than 1.8°F (1°C) in many parts of the Southwest over the last 110 years, with isolated 3.6°F (2°C) increases ...
The Climate of the Last Millennium
The Climate of the Last Millennium

... of this region, conditions today are the driest they have been throughout the Holocene. By contrast, lakes of inland drainage on the Altiplano of Peru and Bolivia have expanded and increased in depth from the mid-Holocene to the present. Lake Titicaca, for example, is currently close to its highest ...
The Mid-Atlantic Region and its climate: past, present
The Mid-Atlantic Region and its climate: past, present

... oceans and estuaries. This zone traverses all of Delaware and parts of New Jersey, Maryland, Virginia, and North Carolina. The Piedmont is the foothills region covering the eastern, lower portion of the Appalachian mountain range. This area is composed mostly of metamorphic and igneous rock, and cov ...
Overlooked Science Issues in Climate Change
Overlooked Science Issues in Climate Change

Climate change variables in relation to direct
Climate change variables in relation to direct

... Further examples: respondents’ reported experiences of environmental changes and events  “Well during the 50s 60s and 70s gully buster storms came from the sw every afternoon 3pm 5pm and dump 1-2 inch rain and disappear they only occasionally happen now” (Ballina, NSW).  “I live in bushland and h ...
What is climate change?
What is climate change?

... concentrations have increased so dramatically • Deforestation contributes to rising atmospheric CO2 - Forests serve as reservoirs for carbon - Removing trees reduces the carbon dioxide absorbed from the atmosphere • Human activities increased atmospheric CO2 from 280 parts per million (ppm) to 389 p ...
Global Climate Change - A Suggested Resources list
Global Climate Change - A Suggested Resources list

... content issues: change over time, production, reduction… http://www.globalwarmingart.com/wiki/Carbon_Dioxide_Gallery Carbon for Kids – a series of four images that convey the relationship between a young person and carbon production in the United States. http://www.icbe.com/carbonforkids/ Climate Ac ...
Global Climate Change and the Risks to Coastal Areas from
Global Climate Change and the Risks to Coastal Areas from

... blame were not difficult to identify. They included local governments, the governments of the states located along the Gulf Coast, the Army Corps of Engineers, high-ranking officials in the Department of Homeland Security and Federal Emergency Management Agency, and the President of the United State ...
climate change, causation, and delayed harm
climate change, causation, and delayed harm

... the “thermal inertia” of the oceans.5 Because water has a high heat capacity, it takes much longer to heat up than the atmosphere does. Accordingly, it will take decades or even centuries for the full impacts of historic greenhouse gas emissions to be felt in changes to global temperature levels, se ...
6-4 Charting a Course for the Future
6-4 Charting a Course for the Future

... a. a decrease in the amount of heat that reaches the surface. b. a decrease in the amount of UV radiation that reaches the surface. c. an increase in the amount of rainfall. d. an increase in the amount of UV radiation that reaches the surface. Slide 21 of 30 End Show Copyright Pearson Prentice Hall ...
Climate Change Vulnerability Assessment and
Climate Change Vulnerability Assessment and

... resiliency and management of public infrastructure, as well as stress natural shorelines and Sarasota Bay. Storm surge associated with extreme storms and seasonally-high “King Tides” poses an immediate and credible threat to our community as tides surge increasingly higher and extend further inland. ...
Climate Change
Climate Change

... Here’s an infrared (IR) one Notice that the IR one has a longer wavelength again It also has much less energy – but it’s IR that is of interest to us ...
Chapter 18 - Santa Rosa Home
Chapter 18 - Santa Rosa Home

... concentrations have increased so dramatically • Deforestation contributes to rising atmospheric CO2 - Forests serve as reservoirs for carbon - Removing trees reduces the carbon dioxide absorbed from the atmosphere • Human activities increased atmospheric CO2 from 280 parts per million (ppm) to 389 p ...
Climate Change and Coral Reefs By: Maddie Renner
Climate Change and Coral Reefs By: Maddie Renner

... a greenhouse) since the heat can’t escape to space. These “greenhouse gases” include carbon dioxide, water vapor, methane, nitrous oxide, and chlorofluorocarbons. ...
12169008
12169008

... significant role in the analysis and interpretation of data from crucial research and development programmes operating in the country. The jobs assigned to me were quite challenging and exercised my organizational, time management, analytical and research skills. This internship report will first fo ...
Uncertainties in future projections of extreme precipitation in the
Uncertainties in future projections of extreme precipitation in the

climate change impacts in kerala-an overview
climate change impacts in kerala-an overview

... • As per INCCA report(2010), yields of coconut are projected to increase in the west coast of India (includes kerala) by up to 30% due to temperature increase. • Increase in coconut yield IN THE WEST COAST may be mainly attributed to projected increase in rainfall (~10%) and relatively less increase ...
The Relationship between Land–Ocean Surface Temperature
The Relationship between Land–Ocean Surface Temperature

The scientific consensus on climate change: How do we know we`re
The scientific consensus on climate change: How do we know we`re

... Roughly 15% of the papers dealt with methods, and slightly less than 10% dealt with paleoclimate change. The most notable trend in the data is the recent increase in such papers; concerns about global climate change have given a boost to research in paleo-climatology and to the development of method ...
Smith et al (2009
Smith et al (2009

Future climate warming and changes to mountain permafrost in the
Future climate warming and changes to mountain permafrost in the

... Permafrost is defined as ground which remains at or below 0 °C for at least two consecutive years (Harris et al. 2003). Although the environmental conditions suitable for permafrost exist in most mountainous regions of sufficient elevation (Travassos et al. 2008; Viviroli et al. 2011), present under ...
Comment by:  Patrick J. Michaels and Paul C. Knappenberger
Comment by: Patrick J. Michaels and Paul C. Knappenberger

... incorporate the SCC, a clear distinction should be made between domestic costs/benefits and foreign cost/benefits—and numerical calculations of each provided in all cost/benefits analyses included in the proposal (to be included in the main body of the proposal). In this way, the public can readily ...
Working Paper 217 - Bettis et al 2016 (opens in new window)
Working Paper 217 - Bettis et al 2016 (opens in new window)

The amplitude and phasing of climate change during the last
The amplitude and phasing of climate change during the last

... records from the Mindanao Sea, TR163-19 and core V2130, in the western and eastern equatorial Pacific, respectively. The offset between Sulu Sea SST and d18Oruber is consistent with observations from other equatorial Pacific sites and reflects changes in hydrology. Within dating uncertainty, the equ ...
PDF
PDF

... so the warming during the past 30 years cannot be attributed to an increase in solar energy reaching the Earth. The frequency of volcanic eruptions, which tend to cool the Earth by reflecting sunlight back to space, also has not increased or decreased significantly. Thus, there are no known natural ...
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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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