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Arctic and Antarctic end-of-season report – October 2021

August until the minimum sea ice extent in mid-September, melting returned to above-average levels, associated with degradation of the ice in the Beaufort and Chukchi Seas. Figure 5. 3-week running mean sea ice extent change for 2021 (red), compared to 2020 (dark blue), previous years from 1979 (light

wiser0172_entebbecommsworkshop_20190327.pdf

AND APPLICATIONS CENTRE (ICPAC) W2SIP/NECJOGHA Greater Horn of Africa Climate Communication Workshop GHACOF51, ENTEBBE, UGANDA 9 th – 10 th FEBRUARY 2019 Program 8 th February 2019 Arrival of Participants and Check in Day One: Saturday February 9 th 2019 8:00-9:00 Arrival and Registration

PowerPoint Presentation

international modelling centres. Much More Likely Below Normal Near-Normal Above Normal Likely Likely Much More Likely Climate Outlook Africa: November to August Overview 5 Global Outlook - Rainfall Outlook: El Niño-Southern Oscillation (ENSO) – Whilst oceanic indicators, including sea surface temperatures

PowerPoint Presentation

(November-January). However, other centres (such as BoM) have predictions which are much more finely balanced between ENSO-neutral and La Niña. Clearly, there is some uncertainty with predictions. Most likely is that ENSOneutral conditions will persist for the next couple of months, with any transition

PowerPoint Presentation

Climate Prediction Centre / NCEP statement (PDF) stating that: “There is a ~60% chance of a transition from La Niña to ENSO-Neutral during the Northern Hemisphere spring 2021 (April-June).” Despite this trend La Niña will continue to be a dominant driver of rainfall patterns, especially in the tropics

Benoît Lavraud

propagation in the inner heliosphere? • High cadence white light imaging in low corona (1.15 – 4 Rs) for CME acceleration • Wide angle heliospheric imagers to track CME/CIR interactions in heliosphere • Polarization information for accurate trajectory • Off-Sun-Earth line location for tracking

asia-climate-outlook---september-2023-v2.pdf

shading represent values above the 80th (Warm) and 90th (Hot) percentile, respectively; regions shaded in light and dark blue indicate values below the 20th (Cool) and 10th (Cold) percentile, with respect to the 1981-2010 climatology. The data used in this map are from the NOAA Climate Prediction Center

150414 International Consultation FINAL

PWS International Products Consultation Executive Summary Although this was a fairly light touch consultation due to limited Secretariat resources, the evidence in this report is enough to be able to give some broad conclusions to the questions posed: 1. Are the current international services

james_tappin-on_the_importance_of_polarisation.pdf

have had polarizers since the days of C/P on SMM and SOLWIND on P78-1. – This capability has tended to be underused. Mainly because of low cadence. Polarization at Large Elongations. ● ● High degree of polarization of Thomson-scattered light to well past 90°. Current imagers are not noise-limited

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