Instructors of Record: Dr, Vladimir Alexeev (474-6430, valexeev@iarc.uaf.edu) & Dr. Uma Bhatt, (474-2662, bhatt@gi.alaska.edu)
Meeting Time: 3:30-4:30 p.m. on Friday in IARC 319 (with some exceptions)
Office Hours: By appointment
Prerequisites: Graduate Standing and a basic knowledge of meteorology and/or oceanography, climate, such that the student is able to read and comprehend current journal articles reasonably well.
Materials Needed: No Required Text. Reading materials will be available for students/participants to copy.
Expectation and Grading Policy: Students are expected to attend the class, do the required reading, and participate. Each student will lead a discussion for at least one journal article or give a research talk. The class will be graded Pass/Fail.
The "Climate Group" is an informal meeting for researchers, Ph.D. and Masters students to be held at IARC. The meetings will include both progress reports on ongoing research and journal paper discussions.
The main interests include topics in:
New (including very raw) ideas, interesting articles, formal and not so formal presentations by locals and visitors will be on the agenda. Participating students will be exposed to a free format discussion of modern ideas in climate related disciplines.
All students are encouraged to contribute and students taking the course for credit are required to lead at least one discussion during the semester. This may include either presenting a research plan, research results, or leading a discussion of a journal article.
This semester the course reading will be loosely structured around the following three topics:
DATE |
TOPIC |
MEETING ROOM & Snack |
---|---|---|
3 Sept. 2004 |
|
IARC
319 |
10 Sept. 2004 |
|
IARC
319 |
17 Sept. 2004 |
Special Guest Speaker: Dr. Kurt Cuffey, details below |
IARC 407 |
24 Sept. 2004 |
Stommel Box Model Paper (Led by B. Hibler) Please READ before class (See Bill to get copies if you did not get them last week):1) Thermohaline
Convection with Two Stable Regimes of Flow, by H. Stommel, Tellus,
1961, p 224-230
|
IARC
319 |
1 Oct. 2004 |
Paper discussion: Giannini et al. 'The preconditioning role of TAV in the development of the ENSO teleconnection: implications for the prediction of Nordeste rainfall', Climate Dynamics, 2004 - Discussion led by K. Sterling |
IARC
319 |
8 Oct. 2004 |
"A Model Ensemble Assessment of the Enhancement of Arctic Warming by Sea Ice Retreat" (Research Talk by Colin Murray) |
IARC
319 |
15 October 2004 |
Climate Predictability Overview (V. Alexeev) Papers
related to this topic:
|
IARC
319 |
22 October 2004 |
Sensitivity to Resolution in the ARPEGE Climate Model (M. Rawashan) |
IARC
319 |
29 October 2004 |
Hurricanes Now and in the Future (John Walsh) |
IARC 319 |
5 November 2004 |
Overview of the Ocean Thermohaline Circulation (H. Simmons) |
IARC
319 |
12 November 2004 |
Question
to be explored this week (Think about it before class):
|
IARC 319 |
19 November 2004 |
Paper
discussion: Marshall, John; Schott, Friedrich 1999 |
IARC 319 |
3 December 2004 |
Paper Discussion: C. Mauritzen and S. Häkkinen,
On the relationship between dense water formation and the "Meridional
Overturning Cell" in the North Atlantic Ocean, Deep Sea Research Part
I: Oceanographic Research Papers, Volume 46, Issue 5, May 1999, Pages 877-894. |
IARC 319 |
10 December 2004 |
Paper
Discussion: T. Schmith , & C. Hansen, " Fram
Strait Ice Export during the Nineteenth and Twentieth Centuries Reconstructed
from a Multiyear Sea Ice Index from Southwestern Greenland" |
IARC 319 |
Prof. Kurt Cuffey, University of California Berkeley (Speaker 17 Sept. 2004 )
Analyses of stable isotopes in polar precipitation are an important tool for the global environmental sciences and for studies of polar regions. The venerable history of these analyses is widely recognized but misconceptions about stable isotope systematics and the proper use of stable isotopes are also common. In a series of two lectures, I will discuss (at a general level) the physical controls on the stable isotopic composition of polar precipitation, from the molecular scale upward through the meso-scale to the planetary scale. Next, the usefulness of stable isotopes in ice cores as climatic indicators will be evaluated. Finally, I will show how stable isotopes have been used, in conjunction with other tools, to establish some of the most significant findings of environmental geophysics: the role of biogeochemistry in global climate changes, the sensitivity of global climate to forcings, and the capacity of our planet's climate to change rapidly. A bibliography will be provided for those interested in more extensive exploration of the topics.