NCAR/UCAR/UOP

Atmospheric Research - NCAR & UCAR
NCAR UOP UCAR
photo Home Our Organization Our Research News Center Education Community Tools Libraries

 

Understanding Climate Change

Multimedia Gallery

From Global Warming to Regional Effects | Impacts on Natural Systems | Global Warming FAQs | Multimedia Gallery

Media Types

line separator

Scientific Visualizations   Webcasts

simulation

Climate Change Simulation, 1870–2100
This animation depicts global surface warming as simulated by the NCAR-based Community Climate System Model (CCSM). It shows warming and cooling compared to average temperatures at the end of the 19th century. (These departures from the average are called temperature anomalies.) The map shows warming and cooling over the entire globe; the graph displays the global average temperature, year by year. Several major volcanic eruptions (such as Agung on the island of Bali in 1963) are noted in the graph and the subsequent cooling is seen in the animation. Click here to open a Web page where the animation can be launched in a variety of formats. (©UCAR. News media terms of use*)

 

Kevin Trenberth

NCAR scientist discusses IPCC report
Kevin Trenberth, a senior scientist at NCAR and one of the major authors of the 2007 assessment by the Intergovernmental Panel for Climate Change, explains why the IPCC reports are an authoritative source of climate change information. The IPCC, a group representing over 180 governments, conducts assessments of global climate change by hundreds of scientists who are experts in the field. It operates under the auspices of the U.N. Environment Programme and the World Meteorological Organization. Click here or on the image to launch the webcast. (©UCAR; running time: 4 minutes. News media terms of use*)

ipcc globes

Dual-globe View, Climate Change Simulation, 1870–2100
This animation depicts global surface warming as simulated by the NCAR-based Community Climate System Model (CCSM). It shows warming and cooling compared to average temperatures at the end of the 19th century. (These departures from the average are called temperature anomalies.) The greater difference from average at the poles is due to "polar amplification," a warming feedback loop as sea ice melts, warm water migrates poleward, and open water absorbs more sunlight. Click here or on the image to open a Web page where the animation can be launched in a variety of formats.
(©UCAR. News media terms of use*)

 

Climate Future

Climate Future: Voices of Science
Some of NCAR's most prominent scientists weigh in on key questions about climate change in these short interviews, produced by NCAR Education and Outreach. Click here or on the image to open a Web page where the webcast can be launched. (©UCAR. News media terms of use*)

sea ice

Arctic Sea Ice, Summer Minimum, 1990–2049
This animation, based on simulations produced by the NCAR-based Community Climate System Model, show the year-to-year variability of Arctic sea ice. For much of the 20th century, the model accurately captures the expansion and contraction of the area covered by sea ice from one late summer to the next, based on natural climate cycles. By the end of the 20th century, however, the ice began to retreat significantly because of global warming.

Within a few decades or sooner, the model simulations show that the ice is likely to shrink abruptly, losing about two-thirds of its area over the course of about a decade. By about 2040, the Arctic may be nearly devoid of sea ice during the late summer unless greenhouse gas emissions are significantly curtailed. Click here or on the image to open a Web page with two stills and the animation, which can be launched in a variety of formats. (©UCAR. News media terms of use*)

 

weather modification

More Climate Webcasts
Over 75 webcasts dealing with climate science and science policy are available. Click here or on the image to open a Web page with a listing of all climate-related webcasts. (©UCAR. News media terms of use*)

line separator

back to top

Future Climate Change Impacts, by Region

world map


View an interactive map of potential impacts of climate change. The selected impacts are based on the region-by-region analysis conducted by IPCC Working Group II. The IPCC has assigned "high confidence" to these projected impacts unless otherwise stated. Click here or on the image to open a Web page with the enlarged, interactive map as well as a text version suitable for printing. (©UCAR. News media terms of use*)

line separator

back to top

Images to explain climate modeling
The increasing level of detail in climate models

This illustration shows how the amount of detail in climate models has increased in recent years, largely because of the calculation power provided by newer supercomputers. In the 1990s, high-resolution global climate models operated on the T42 resolution scheme (upper left). At this resolution, temperature, moisture, and other features were tracked in grid boxes that each spanned about 200 by 300 kilometers at midlatitudes (120 x 180 miles), an area roughly as large as West Virginia.

In more recent modeling that led up to the 2007 IPCC Working Group I report, the NCAR-based Community Climate System Model (CCSM) routinely operated at T85 resolution (upper right), with midlatitude grid points of about 100 by 150 km (60 x 90 miles)—the size of Connecticut.

Better resolution not only provides a more true-to-life depiction of atmospheric processes, but also allows for more realistic topography, which makes regional climate projections more accurate. For example, the highest Rocky Mountains appear as two coarse grid points at T42 but as a more diverse assortment of high peaks at T170 (lower left). Enhancements in computing power will help scientists explore the use of higher resolutions, such as T170 and T340 (lower right). Click here or on the image to enlarge. (Illustration courtesy Warren Washington, NCAR. ©UCAR. News media terms of use*)

 

3-D view of CCSM components - ocean, land, water cycle, sun

Now in its third generation, the NCAR-based Community Climate System Model (CCSM) is one of the world’s most sophisticated and widely used models of global climate. This graphic illustrates the many components included in the CCSM, ranging from cirrus and stratus clouds to ocean currents and soil moisture. These components are also typical of many of the dozen or so climate models at other major research centers around the globe. Click here or on the image to view a larger image with more details on each component. (Illustration by Paul Grabhorn, ©UCAR. News media terms of use*)

 

 

 

The increasing level of detail in climate models
The complexity of global climate models has increased enormously over the last 20 years, as shown in this flow chart. Beneath each time period is a list of the components included in state-of-the-art models such as the NCAR-based Community Climate System Model. Click here or on the image to enlarge. (Illustration courtesy Warren Washington, NCAR. ©UCAR. News media terms of use*)

line separator

back to top

Photos from the UCAR Digital Image Library - click on an image for description, credit, and high resolution files

bogs
sea ice
drought
flood
flood
erosion
drought
fire

 

Find more photos and stock video footage in the UCAR Digital Image Library.

back to top

Updated:March 2008


*News media reproduction to illustrate this story and nonprofit use permitted with proper attribution as provided above and acceptance of UCAR's terms of use. Find more images in the UCAR Digital Image Library.

The University Corporation for Atmospheric Research manages the National Center for Atmospheric Research under sponsorship by the National Science Foundation. Any opinions, findings and conclusions, or recommendations expressed in this publication are those of the author(s) and do not necessarily reflect the views of the National Science Foundation.

This document can be found at
rss icon Subscribe to NCAR & UCAR RSS feeds at http://www.ucar.edu/news/rss

 
 
(Winter-Spring 2007)