PPT-Activating Strategy : Watch Ice Age:

Scrat Continental Crack Up video clip and have students either answer individually or with a partner the following questions 1 Which parts of Scrats adventure is accurate . Michael . Dutter. and Todd . Kluber. NOAA/National Weather Service Marquette, . MI. 2014 Great Lakes Operational Meteorology Workshop – Ann Arbor, MI. Despite Lake Superior being completely (or nearly completely) ice covered for much of Feb-April 2014, lake effect bands were still occasionally observed. Some of these proved to be relatively significant.. S. ubstituted Benzenes. How do we know where E. +. will substitute?. In general, consider:. Orientation. Z is either an . ortho,para. -director or a . meta-director. Rate. Z is either activating (the rate of reaction is faster than benzene) or deactivating (the rate of reaction is slower than benzene). Wiliam. Embedding . Formative Assessment: . Practical Techniques for K – 12 Classrooms. “Nothing has promised so much and has been so frustratingly wasteful as the thousands of workshops and conferences that led to no significant change in practice when teachers returned to their classrooms.”. . Robert LaPlante. NOAA/NWS Cleveland, OH. David Schwab. Jia. Wang. NOAA/GLERL Ann Arbor, MI. 15 March 2012. Outline. Description of the expansion of the GLIM to all five Great Lakes for the 2011-2012 ice season. Zhibo (. zippo. ) Zhang. 03/29/2010. ESSIC. Outline. Background. Importance of ice cloud. Ice particle model and ice cloud retrieval. Influence of ice particle model on . t. retrieval. Comparison of MODIS and POLDER ice . The Ice Age. Man Flourishes. 15,000-10,000B.C.E. .. Essential Standard. 6.H.2- Understand the political, economic and/or social significance of historical events, issues, individuals and cultural groups.. What impact do you think Prince Henry had on the Age of Exploration? Why is he important?. What were the three major Causes of Exploration? Why do you think they lead to the Age of Exploration?. On the Agenda. Sea Ice Formation. --in Antarctica, begins forming in late summer with winds from the. . continent, evaporative cooling at ocean surface reduces . . water temperature to ~-1.8 °C. --as water temperature falls, ice crystals of fresh water begin . Hint, don’t forget to find the volume of the ice first!. ). Warm Up: Density of Ice. Does the density of ice you calculated make sense? Why or why not?. Warm Up: Density of Ice. Draw a dot diagram to compare the density of ice and water.. Temperature. The mixing time mainly influences the speed and duration of the . foaming. It also improves the stability of the foams. The process temperature influences the starting time, duration and speed of foaming at high SiO. Navigating. Navigating ocean currents and ice drift. In the past many people did not know that there was ice in the Arctic Ocean or that the ice moved. . We first learned this from finding objects that had drifted across the Arctic.. . Albedo increases due to more ice coverage to something like about 0.35 which is then equivalent to a 6% change (3 % change in mean geometric distance from the Sun). Qualitative Albedo Feedback loop:. JPL’s . ISSM (Ice Sheet and Sea Level System Model). shows how the loss of ice mélange makes it easier for rifts in the ice to widen (. ice mélange and rifts shown in pink). Ice mélange remnants . Yoel Kortick. Senior Librarian. Introduction. Excel file from the vendor. Activating the portfolios from the Excel sheet. Fixing the Excel sheet so all portfolios will be activated. 3. Introduction.