PPT-El Nino versus the Blob – is
Author : tatyana-admore | Published Date : 2018-11-12
Spouthern California Facing more drought Chris Funk Research Director Climate Hazards Center Chris Funk USGSUCSB Climate Hazards Group Warming shifts the mean of
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El Nino versus the Blob – is: Transcript
Spouthern California Facing more drought Chris Funk Research Director Climate Hazards Center Chris Funk USGSUCSB Climate Hazards Group Warming shifts the mean of distributions causing more extreme events. El Nino conditions are characterized by above normal sea surface temperatures near the equator in the eastern and central portions of the equatorial Pacific Ocean While these conditions exist many thousands of miles away from Iowa impacts from El Ni Achieving scale covariance. Goal: independently detect corresponding regions in scaled versions of the same image. Need . scale selection. mechanism for finding characteristic region size that is . covariant. Wednesday . 1/30. Weather vs. Climate. Weather. Instantaneous description of what the atmosphere is doing at a particular time and place. Climate. Description of what weather is usually like in a region (large or small).. FACTS and . FIGURES. Esther Lieu. Feb 2012. WHY IS THERE SO LITTLE DATA ON NATIONALITY OF BENEFITS CLAIMANTS?. The DWP said, in response to a Parliamentary Question, that whilst . n. ationality is a factor for residence-based benefits, once residence is established, . keypoint. detection. D. Lowe, . Distinctive . image features from scale-invariant . keypoints. ,. . IJCV. 60 (2), pp. 91-110, 2004. . Keypoint. detection with . s. cale selection. We want to extract . The following presentation was used to review for the test.. 9. -17-15. topics. . .. Density. Salinity. Ocean currents. Conveyor Belt. El . N. ino. What to study . . .. Notebook entries. Lab: Density. Nino Events. Chip Konrad. Director of the NOAA Southeast Regional Climate Center. University of North Carolina at Chapel Hill. A. cknowledgement: Jordan McLeod, the new regional climatologist at SERCC. Overview. The Slab Ocean El Nino. How good are the CMIP models?. Non-linearity. Seasonality (spring barrier). CP vs. EP. Teleconnections delayed feedback. Climate Change. Overview. The Slab Ocean El Nino. Michelle L’Heureux (. NOAA CPC). ENSO Forecast team (A. . Barnston. , E. Becker, G. Bell, T. Di . Liberto. , J. Gottschalk, M. . Halpert. , Z. Hu, N. Johnson, W. Wang, Y. . Xue. ), M. . Tippett. Niño-3.4 Forecasts from the NMME. Walker circulation. ) that typically finds rising air and heavy rain over the western Pacific and sinking air and generally dry weather over the eastern Pacific. When the trades are exceptionally strong, water along the equator in the eastern Pacific becomes quite cool. This cool event is called La Nino . Which Will Win and How Will This Affect the 2016 Season?. https://youtu.be/WtneCL8iA2A. PDO. Pacific Decadal Oscillation. Topics:. Definitions – What are we talking about here?. Present status of El Niño, The Blob, PDO – Which is ‘winning’? Global Warming?. Pages 484-487. EL NINO. . Go to this website and read this background information first:. http://oceanservice.noaa.gov/facts/ninonina.html. You may need to come back to this website to fill in any notes that you missed. pulser. ). B. Quinn. Feb. 23, 2018. 1. Cabling scheme for . HCal. One signal, one HV cable to each tube. (Plus one HV & 6 signal/section for . pulser. ). Cables secured, strain-relieved on gantry behind . Bedo tye nino ducu i ot kwan pire tek
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