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Climate Change and Extreme Weather
Climate Change and Extreme Weather

... Hansen, J., M. Sato, and R. Ruedy, 2012: Perception of climate change. Proc. Natl. Acad. Sci., 109, 1472614727, E2415-E2423, doi:10.1073/pnas.1205276109. IPCC, 2012: Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation. A Special Report of Working Groups I and II o ...
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ATMOS 5400: The Climate System 01. Introduction
ATMOS 5400: The Climate System 01. Introduction

... Goals of this course • The purpose of this course is to provide you with scientific understanding of Earth's climate system. • Our goal is to understand how climate depends on physical processes within, and interactions among, five climate system components: atmosphere, oceans, land surfaces, biosp ...
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The Commonwealth and Climate Change,West Bengal, Jan 2010
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... reaction. It is considered irresponsible for a doctor not to have epinephrine in his or her medicine cabinet. Note, however, the comment of James Lovelock (Gaia): Geoengineering today is “comparable with 19th century medicine.” Two thrusts for research: Deployment engineering (e.g., avoid coagulatio ...
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Statement of relevance to the NOAA climate science and services

... processes that control the climate system’s response to radiative perturbations. We focus on coupled interactions between the atmospheric dynamics, large scale radiation, ocean circulation and the cryosphere recognizing the inherent inter-connectedness of the subcomponents of the climate system. We ...
Feb 27 RK - University of San Diego
Feb 27 RK - University of San Diego

... Sunspots are magnetic storms that appear as dark patches on sun’s surface Number and size are maximal every 11 years Solar output ca. 0.1% higher than normal during maxima ...
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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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