PPT-Operational transition of combined ENSO, MJO, and trend inf

Nat Johnson 1 and Dan Harnos 2 Stephen Baxter 23 Steven Feldstein 4 Jiaxin Feng 56 Michelle LHeureux 2 and ShangPing Xie 5 1 Cooperative Institute for Climate Science Princeton University. Definition The MJO is an intraseasonal fluctua tion or wave occurring in the glob al tropics The MJO is responsible for the majority of weather variability in these regi ons and results in variations in several important atmospheric and oceanic par Fig. 3: As in Fig. 2, but at ten days after convective initiation.. Preferred ENSO Phase within Each Composite. Fig. 1: Histogram of ONI (°C) for (a) real MJOs and (b) failed MJOs. The sample size, mean, and standard deviation of each subset are provided in the top left corner of each histogram.. C. hanging Climate. CLIVAR Research Focus Group. Co-chairs: Eric Guilyardi (IPSL, NCAS-Climate), Andrew Wittenberg (GFDL) . With contributions from:. Mat Collins (Uni Exeter), Wenju Cai (CSIRO), Tony . SO442 Lecture 9/30/2013. B. Barrett. http://blogs.wpri.com/2013/08/21/why-hurricane-season-may-start-to-pick-up/. . First, atmospheric oscillations. The weather we notice here in Annapolis today is really the combination of many atmospheric oscillations. over the Central Indian . Ocean as seen by the TRMM PR. Hannah C. Barnes. Robert A. Houze, Jr.. University of Washington. MJO Field Data and Science Workshop. 5 March 2013, . Hapuna. Beach Resort, . Webinar . Series. Dynamics of the Madden-Julian Oscillation Field Campaign. Climate Variability. . & Predictability. Application of DYNAMO/AMIE observations to validate and improve the representation of MJO initiation and propagation in the NCEP CFSv2. Factors affecting forecast skill of the MJO over the Maritime Continent. Augustin Vintzileos. CPC/NCEP . – . CICS/ESSIC. , University of Maryland College . Park. Jon . Gottschalck. CPC/NCEP. Problem statement:. Oscillations . . 伴隨季內震盪的. 雲. 水. 過程. 分析. Chung-. Hsiung. Sui . Dept. of Atmospheric Sciences . National Taiwan . University. 隋中興 洪竟書. . 曾開智. . 台灣大學大氣科學系. Observation and Simulation . Yongqiang Sun, Michael Ying, . Shuguang. Wang, . Fuqing. Zhang. Group meeting. 07-19-2013. Wheeler and . Kiladis. . 1999. . . Kiladis. . et al. 2009. 2-Day. Motivation: . .”. Model composites (method . etc. ) 6 slides. Comparison real time forecast to those composites. ENSO Precipitation and Temperature Forecasts in the NMME: Composite Analysis and Verification. Li-Chuan Chen. 22030. 2 . Department . of Atmospheric, Oceanic and Earth . Sciences, George . Mason University, Fairfax, VA . 22030. Projected changes of the tropical Atlantic vertical wind shear and its relationship with ENSO in the SP-CCSM4. IGLAUCOMA TODAYISUMMER 2011 COVER STORY (Continued from page 38) SUMMER 2011IGLAUCOMA TODAYI COVER STORY IGLAUCOMA TODAYISUMMER 2011 Incisional surgery is very unlikely to becomethe preferred first l Dialogue initiated in 2016 following the . El . Niño-related emergencies, led by OCHA and FAO, subsequently WFP, WMO, IFRC, START network NGOs and others;. A . structured . framework to ensure . global coordination between IASC partners and relevant development partners at global, regional and national levels, . Workshop on the Tropical Dynamics and the MJO, . Honolulu, January 14-15 2014. Understanding of essential dynamics of the MJO. MJO. –. a Dynamic Definition . An equatorial . planetary scale . circulation system coupled with a .