OLR is a good measure of convection. Outgoing Longwave Radiation (OLR) area averages over the central equatorial Pacific (160°E-160°W).
The likelihood of ENSO-neutral is estimated to be about 40% and that for El Niño near-zero. This is because heat energy available at the ocean surface is extracted by storms passing over them and used as fuel for their intensification. Composition and Structure, Atmospheric It is calculated using the ICOADS dataset.
Total SSTs also available for this region. Calculated from the Monthly NOAA ERSST V5 (at NOAA/CPC).
Correlates well with teleconnections to North America. The following indices all help characterize ENSO but at different
Composite Rainfall of ENSO for Individual Stations; Correlation Between ENSO Index and Rainfall; Spatial Distribution Maps of Rainfall Percentile; Annual Cycle of Average Seasonal Rainfall (1955-1996) Seasonal Total Rainfall (millimeters) with ENSO Episodes Noted (1955-1996) Seasonal Total Rainfall (Percentile) with ENSO Episodes Noted (1955-1996)
Correlates well with teleconnections to North America.
Total SSTs also available for this region.
If you do not receive an email within 10 minutes, your email address may not be registered, It is the running 3-month mean SST anomaly for the Ni ñ o 3.4 region (i.e., 5 o N-5 o S, 120 o-170 o W).
Neutral Dashboard looking at the current year to neutral events.
Processes, Information Jul 2020 ESPI Precip Index: ENSO Precipitation Index. Outgoing Longwave Radiation (OLR) area averages over the central equatorial Pacific (160°E–160°W). Properties of Rocks, Computational Total SSTs also available for this region. Correlates well with teleconnections to North America. Climatology 1981-2010. Calculated from the Monthly NOAA ERSST V5 (at NOAA/ESRL). Calculated at NOAA/CPC from the GODAS dataset. While El Niño–Southern Oscillation (ENSO) influences eastern North Pacific (ENP) tropical cyclones (TCs) through a variety of atmospheric processes when examined concurrently, ocean pathways dominate at longer lead times.
in Modeling Earth Systems (JAMES), Journal of Geophysical Research Tools. Library, Analysis & Plotting Small Bodies, Solar Systems SST anomalies averaged over the NINO4 region 5°North–5°South; 160°East–150°West (western most of Nino indices). Boulder, CO 80305-3328, Profiler Network Data & Image Calculated from the Monthly NOAA ERSST V5 (at NOAA/ESRL).
The EI and LI are in turn combined to create the ESPI index. Please note: The publisher is not responsible for the content or functionality of any supporting information supplied by the authors. locally and at a distance. Oceanic Niño Index: 3 month running mean of ERSST.v4 SST anomalies in the Niño 3.4 region (5°N-5°S, 120°-170°W) Calculated from the ERSST V5 (at NOAA/CPC).
The index is based on rainfall anomalies in two rectangular areas, one in the eastern tropical Pacific (10°S-10°N, 160°E-100°W) and the other over the Maritime Continent (10°S-10°N, 90°E-150°E). Calculated from the Monthly NOAA ERSST V5 (at NOAA/CPC). There are fewer time series that cover from 1870 to present. Learn about our remote access options, E-mail address: Karthik.Balaguru@pnnl.gov, Pacific Northwest National Laboratory, Richland, WA, USA, Lawrence Berkeley National Laboratory, Berkeley, CA, USA, Department of Geological and Atmospheric Sciences, Iowa State University of Science and Technology, Ames, IA, USA.
Tropical Pacific integrated temperature anomalies (0-300m) 160°E–80°W.
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Produced at NOAA/ESRL PSL. Geophysics, Geomagnetism The sources for various data used in this study are as follows: ENP TC track data—https://www.nhc.noaa.gov/data/, ERA5 data—https://www.ecmwf.int/en/forecasts/datasets/reanalysis-datasets/era5, NCEP‐GODAS ocean reanalysis data—https://www.cpc.ncep.noaa.gov/products/GODAS/, NCEP2 reanalysis data—https://www.esrl.noaa.gov/psd/data/gridded/data.ncep.reanalysis2.html, Hadley SST data—https://www.metoffice.gov.uk/hadobs/hadisst/, ORAS4 ocean reanalysis data—https://icdc.cen.uni-hamburg.de, ONI—https://origin.cpc.ncep.noaa.gov/products/analysis_monitoring/ensostuff/ONI_v5.php, SOI—www.cpc.ncep.noaa.gov/data/indices/soi, MEI—https://www.esrl.noaa.gov/psd/enso/mei/, and ELI—https://portal.nersc.gov/archive/home/projects/cascade/www/ELI, and the program to compute UPI is available online (at ftp://texmex.mit.edu/pub/emanuel/TCMAX/). Calculated at NOAA/CPC.
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