Browse
Search
CFE agenda 111416
OrangeCountyNC
>
Advisory Boards and Commissions - Active
>
Commission for the Environment
>
Agendas
>
2016
>
CFE agenda 111416
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
3/2/2018 11:24:10 AM
Creation date
3/2/2018 11:21:57 AM
Metadata
Fields
Template:
BOCC
Date
11/14/2016
Meeting Type
Regular Meeting
Document Type
Agenda
Document Relationships
CFE minutes 111416
(Message)
Path:
\Advisory Boards and Commissions - Active\Commission for the Environment\Minutes\2016
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
55
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
View images
View plain text
Revised draft (BK/PQ Oct 7, 2016 <br />around the sun. However, orbital changes are not behind today's global warming —our <br />current orbit dictates we should be cooling not warming! CO2 has increased by about 40% <br />since the 1700s from 280 ppm (parts per million) to today's 400 ppm. <br />Ocean acidification is the lesser known result of climate change. The ocean absorbs <br />atmospheric CO2— leading to an increased acidification of the ocean, which is currently <br />30% more acid than 300 years ago (a drop in pH from 8.2 to 8.1). The ocean's ecosystem <br />will begin crashing when pH falls below 7.8. As acidification worsens, it's more difficult for <br />coral to construct reefs and mollusks to calcify their shells. Reef building is particularly <br />vulnerable to climate change —with current loss a sign of that change. If current trends <br />continue all coral reefs will cease to grow, and start dissolving, within 50 years. Australia's <br />Great Barrier Reef has already declined by 50% over the last 30 years. <br />Models <br />Scientists use models to test hypotheses, make predictions, and frame new <br />questions. They test them by replicating observed data. When Global Circulation Models <br />(GCMs) do a good job of replicating past and current observations, we have increased <br />confidence they can forecast the future. GCMs have been able to do just this — including <br />more rapid warming seen since 1950, and short -term cooling after recent volcanic <br />eruptions (Mount Pinatubo, 1991). GCMs also predict many of the extreme events we <br />currently experience, such as major flooding, and extended heat waves and drought. <br />GCMs tell us about the drivers of significant changes in global temperature observed <br />over the last century. Models using only natural forcings (solar variation, volcanic activity) <br />show essentially no temperature increase over the last 100 yrs. When including <br />anthropogenic effects the GCM fit with observed data is very good. Despite skeptics' claims, <br />nobody has created a general circulation model that includes anthropogenic effects <br />explaining climate behavior over the past century without CO2- driven warming. <br />
The URL can be used to link to this page
Your browser does not support the video tag.