PPT-Potential Predictability of Tropical Pacific Ocean

Lauren Stevens and Matt Chamberlain Outline Setup of the experiment Potential predictability of ENSO Potential predictability of airsea CO2 fluxes and Net Primary Productivity Future Work 1. Rockefeller Jr Memorial PKWY Big Hole NB Cowpens NB Fort Donelson NB Fort Necessity NB Moores Creek NB Petersburg NB Stones River NB Tupelo NB Wilsons Creek NB Kennesaw Mountain NBP Richmond NBP Brices Cross Roads NBS Chickamauga and Chattanooga NMP Feb 2014. Jin Huang. Outline:. Global Patterns. Extremes and US anomalies . DJF Climate Attributions. Forecast Verifications. After thoughts on the Monthly Climate Reviews. 2. Global Patterns. Global SST Anomaly (. 1998. -. 99 . decadal shift in global precipitation. Lyon, . Barnston. , DeWitt, . Climate Dynamics . (revised). MAM 2011. PRCP Anomaly. MAM 1999-2011. AVG PRCP Anomaly. East Africa . MAM PRCP Anomaly. vs. . Remote effect. Sourav Taraphdar. 1. Collaborators. :. 1. . Fuqing. Zhang, . Yonghui. . Weng. , Michael (Yue) Ying. 2. . Shuguang. Wang. 3. Juan . Fang. 1. Department of Meteorology, The Pennsylvania State University, . 1998. -. 99 . decadal shift in global precipitation. Lyon, . Barnston. , DeWitt, . Climate Dynamics . (revised). MAM 2011. PRCP Anomaly. MAM 1999-2011. AVG PRCP Anomaly. East Africa . MAM PRCP Anomaly. Introduction to the physical climate system. Oliver . Elison. . Timm. . ATM 306 Fall 2016. Lecture 1. Atmospheric Circulation. Objectives. Objectives. The general circulation of the atmosphere. Winds and pressure systems. Ocean_4_ENSO Lecture. Objectives/Agenda. Objective:. L. earn about El Nino and La Nina the two phases of the ENSO (El Nino Southern Oscillation) . cycle. Apply our understanding to your island. ENSO cycle. Madeline Frank. EAS 4480. Course Project. April 2016. Goals. 4 Ocean Basins:. . North Atlantic, East Pacific, West Pacific, . Indian. Determine the relationship (if any) between active and/or inactive tropical cyclone years among 4 Ocean basins. Lesson 6. What is the MJO?. Large-scale disturbance of deep convection and winds that controls up to half of the variance of tropical convection in some regions. Now known to be a major propagator of weather systems. Geography of storm names. Atlantic . and eastern Pacific. : . “hurricanes” . Indian Ocean and Australia: . “cyclones”. Western Pacific, N. hemisphere: . “typhoons”. Western Pacific typhoons, 2011 . What are cyclones?. This . is . important . when we're talking about ocean storms because the location of the storm determines what we call it. I. f . the storm occurs in the Atlantic Ocean and Northeast Pacific, it's called a hurricane. If the exact same type of storm occurs in the Northwest Pacific, this is a typhoon. And if we find those same storms in the South Pacific and Indian Ocean, these are called tropical cyclones. . Analyses are performed of an ocean-only model driven by observed winds, an idealized atmosphere-only model run with observed SSTs with a uniform tropical warming and an additional warming added to the tropical Indian Ocean, and GOGA and TOGA runs. Kerry Emanuel. Program in Atmospheres, Oceans, and Climate. MIT. Some Issues. What processes control rates of genesis of tropical cyclones?. What processes control the actual and potential intensity of TCs? . Sam Coakley. Advisor: Travis Miles, Ph.D.. Tropical cyclone impact on US. https://. www.ncdc.noaa.gov. /billions/summary-stats. Total cost 1980-2019: $954.4B. Total deaths 1980-2019: 6,507. Tropical cyclone impact on US.