![]() ![]() ![]() On WPC’s surface analyses, this feature is also used to depict outflow boundaries. Trough – an elongated area of relatively low atmospheric pressure the opposite of a ridge. A cold occlusion results when the coldest air is behind the cold front and a warm occlusion results when the coldest air is ahead of the warm front. Two types of occlusions can form depending on the relative coldness of the air behind the cold front to the air ahead of the warm or stationary front. Occluded Front – a composite of two fronts, formed as a cold front overtakes a warm or quasi-stationary front. Stationary Front – a front between warm and cold air masses that is moving very slowly or not at all. Warm Front – a transition zone between a mass of warm air and the cold air it is replacing. Anything that in the judgment of the CWSU forecaster will add value to an existing advisory.Ĭold Front – a zone separating two air masses, of which the cooler, denser mass is advancing and replacing the warmer.To better define hazards expected at a major terminal already within an AWC or AAWU advisory.To define a line of thunderstorms within a larger area covered by the AWC or AAWU advisory.If greater than isolated severe turbulence or icing is occurring, then a new (non-supplementary) CWA should be issued. To upgrade an AIRMET to include isolated severe turbulence or icing. ![]() To upgrade a thunderstorm advisory to include severe thunderstorms.When a hazard has grown significantly outside of the boundary defined by the AWC or AAWU advisory.Volcanic ash, dust storms, or sandstorms.Low Level Wind Shear (surface – 2,000 feet).Conditions meeting convective SIGMET criteria.Phase changes of water Gas, Liquid.When any of the following events are expected to occur within two hours: To learn more about Seneca's privacy practices, visit Privacy Notice. By attending live classes, students are consenting to the collection and use of their personal information for the purposes of administering the class and associated coursework. Live classes may be recorded and made available to students to support access to course content and promote student learning and success. In the event students encounter circumstances that impact their ability to join the platform with their camera on, they should reach out to the professor to discuss. group work, assessments), and high-speed broadband access (e.g. Students joining a live class online may be required to have a working camera in order to participate, or for certain activities (e.g. Flexible Learning spaces are equipped with cameras, microphones, monitors and speakers that capture and stream instructor and student interactions, providing an in-person experience for students choosing to study online. Synchronous (live) classes may be delivered in person, in a Flexible Learning space, or online through a Seneca web conferencing platform such as MS Teams or Zoom. Please visit the Academic Integrity website to understand and learn more about how to prepare and submit work so that it supports academic integrity, and to avoid academic misconduct.Ĭamera Use and Recordings - Synchronous (Live) Classes Section 2.3 and Appendix B of the policy describe various sanctions that can be applied, if there is suspected academic misconduct (e.g., contract cheating, cheating, falsification, impersonation or plagiarism). Ensure that you are aware of Seneca's Academic Integrity Policy which can be found at: Review section 2 of the policy for details regarding approaches to supporting integrity. These values enhance Seneca's commitment to deliver high-quality education and teaching excellence, while supporting a positive learning environment. Seneca upholds a learning community that values academic integrity, honesty, fairness, trust, respect, responsibility and courage. ![]()
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