PPT-Anthropogenic Climate Change, Part one:

The settled issues Topics Definitions An absurdity which needs to be addressed What has been established What is at issue Science The Scientific Consensus Some common challenges to anthropogenic climate change and why they fail. UNSETTLED SCIENCE. Presented to the . Lyncean. Group 24 February 2010. by. Hugh Kendrick. OUTLINE. GREENHOUSE GAS PHYSICS. TEMPERATURE RECORDS. TEMPERATURE PREDICTIONS. CO2 RECORDS. WEATHER TRENDS. Greenhouse Effect. Anthropogenic Greenhouse Effect. “The enhancement of the natural greenhouse effect due to human activity.”. The Problem:. The increase in greenhouse gas levels may trap more IR in the atmosphere, increasing the average global temperature.. Physics Today August 2002 30-36. 01/23/15. Mean . D. = 0.4. ‰. Compare 1970 with 1990. Change in profiles of . d. 13C. f. rom 1970 to 1991. Need depth integrated. c. hange in global ocean. d. 13C. GREETINGS. THE PRINCIPAL. VICE PRINCIPAL -ACAD. VICE PRINCIPAL -ADM. TEACHING STAFF MEMBERS. NON TEACHING STAFF MEMBERS. INVITED QUESTS. ALL STUDENTS. LADIES AND GENTLEMEN. I CONSIDERED IT AS A GREAT HONOUR AND PRIVILEGE TO HAVE BEEN ALLOWED ME TO SPEAK ON. Climatology. is . the study of Earth’s climate and the factors that affect past, present, and future climatic changes.. Climate describes annual variations of temperature, precipitation, wind, and other weather factors.. Comparing EPA estimates to . CAMx. PSAT for 2011. Natural vs Anthropogenic contributions to IMPROVE aerosol extinction. Pat Brewer (NPS), Gail Tonnesen (EPA Region 8), Tom Moore (WESTAR-WRAP). April 2018. 17 January 2011. How and Why Does Climate Change?. Climate changes over a broad range of time scales. Years, decades, centuries, millennia. Many factors combine to affect climate. Variability of incoming solar radiation. Who can forget those moments when something that seems turns out to be vitally even dangerously alive As when an arabesque in the pattern of a carpet is revealed to be a dogs tail which to a nipped an long-term weather patterns. for a particular area.. On Earth we have different climates depending on where you are. . Can you think of any  different climates?. 2. What is climate change?. Climate change. Nitrous . Oxide (N. 2. O). : The Dominant Ozone-Depleting Substance Emitted in the 21. st. . Century, A. . R. . Ravishankara, John S. Daniel, and Robert W. . Portmann, . SCIENCE. , . Vol. . 326, Pages: 123-125, 2009 (OCT 2. Cs-137 and Cs-134 in Ground-Level Air Samples by IMS Stations. Located on the African Continent . . . Ms. Dorice Rashid Seif. 1 . and Mr. Martin Kalinowski. 2. P2.4-307. 1. Examples of the both fine-scale and larger-scale signature of climate and climate history include:. Effect of differences in climate on landforms . Relict . topography formed by now inactive . processes.. Lecture 3 – . Forcings. and Feedback. Outline of course. Do we understand the science behind climate change?. Historical climate. Basics of climate science. Modeling the climate. Understanding the . . Stability. Daniel Osorio, . financial. . stability. . department. , central . bank. . of. . colombia. October. 1st, 2020. 1. Climate Change: Risks to Financial Stability (Carney, 2019). Transition.