Climate Indices: Monthly Atmospheric and Ocean Time-Series
Please reference time series use in publications! Time series that are regularly updated have a * after their name.
| PNA | Pacific North American Index*: From NOAA Climate Prediction Center (CPC) |
| EP/NP | East Pacific/North Pacific Oscillation: From NOAA Climate Prediction Center (CPC). This index replaces the old EP index which is no longer maintained by CPC. |
| WP | Western Pacific Index* From NOAA Climate Prediction Center (CPC) |
| EA/WR | Eastern Asia/Western Russia From NOAA Climate Prediction Center (CPC) |
| NAO | North Atlantic Oscillation* From NOAA Climate Prediction Center (CPC) |
| NAO (Jones) | North Atlantic Oscillation From CRU
Hurrell, J.W., 1995: Decadal trends in the North Atlantic Oscillation and relationships to regional temperature and precipitation. Science 269, 676-679. Jones, P.D., Jónsson, T. and Wheeler, D., 1997: Extension to the North Atlantic Oscillation using early instrumental pressure observations from Gibraltar and South-West Iceland. Int. J. Climatol. 17, 1433-1450. |
| SOI* | Southern Oscillation Index From NOAA Climate Prediction Center (CPC) |
| Niño 3* | Eastern Tropical Pacific SST (5N-5S,150W-90W) From NOAA Climate Prediction Center (CPC): uses the NOAA ERSST V5 anomalies. Now uses https://www.cpc.ncep.noaa.gov/data/indices/ersst5.nino.mth.91-20.ascii. Mean values also available. |
| BEST* longer version |
Bivariate ENSO Timeseries Calculated from combining a standardized SOI and a standardized Niño3.4 SST timeseries. : Uses the dataset (Hadley SST) is now used to calculate Niño 3.4 timeseries. Most recent data is based on the NOAA OI V2 SST dataset. PSL |
| TNA | Tropical Northern Atlantic Index*
Anomaly of the average of the monthly SST from 5.5N to 23.5N and
15W to 57.5W. HadISST and NOAA OI 1x1 datasets are used to create index. Climatology is 1971-2000. Enfield, D.B., A.M. Mestas, D.A. Mayer, and L. Cid-Serrano, 1999: How ubiquitous is the dipole relationship in tropical Atlantic sea surface temperatures? JGR-O, 104, 7841-7848.AOML and PSL |
| TSA | Tropical Southern Atlantic Index*
Anomaly of the average of the monthly SST from Eq-20S and 10E-30W.
HadISST and NOAA OI 1x1 datasets are used to create index. Climatology is 1971-2000. Enfield, D.B., A.M. Mestas, D.A. Mayer, and L. Cid-Serrano, 1999: How ubiquitous is the dipole relationship in tropical Atlantic sea surface temperatures? JGR-O, 104, 7841-7848.AOMLand PSL |
| WHWP | Western Hemisphere warm pool*
Monthly anomaly of the ocean surface area warmer than 28.5°C in the Atlantic and eastern North Pacific. Based on HadISST and NOAA OI SST (for latest value).
Climatology is 1971-2000. Wang, C., and D.B. Enfield, 2001: The tropical Western Hemisphere warm pool, Geophys. Res. Lett., 28, 1635-1638. AOML and PSL |
| ONI | Oceanic Niño Index From NOAA Climate Prediction Center (CPC). Three month running mean of NOAA ERSST.V5 SST anomalies in the Niño 3.4 region (5N-5S, 120-170W), based on changing base period which onsist of multiple centered 30-year base periods. These 30-year base periods will be used to calculate the anomalies for successive 5-year periods in the historical record. |
| MEI V2 | Multivariate ENSO Index (MEI V2) Time series is bimonthly so the Jan value represents the Dec-Jan value and is centered between the months. Details and current values are PSL's MEI webpage. |
| Niño 1+2 | Extreme Eastern Tropical Pacific SST *(0-10S, 90W-80W) From CPC: uses the NOAA ERSST V5 anomalies. Now uses https://www.cpc.ncep.noaa.gov/data/indices/ersst5.nino.mth.91-20.ascii. Mean values also available. |
| Niño 4 | Central Tropical Pacific SST *(5N-5S) (160E-150W) From CPC: uses the NOAA ERSST V5 anomalies | .Now uses https://www.cpc.ncep.noaa.gov/data/indices/ersst5.nino.mth.91-20.ascii. Mean values also available.
| Niño 3.4 | East Central Tropical Pacific SST* (5N-5S)(170-120W) From CPC: uses the NOAA ERSST V5 anomalies | . Now uses https://www.cpc.ncep.noaa.gov/data/indices/ersst5.nino.mth.91-20.ascii. Mean values also available.
| PDO | Pacific Decadal Oscillation is the leading PC of monthly SST anomalies in the North Pacific Ocean. UPDATED: Using data from 1948 to 2002. Details and more information are available. |
| TPI(IPO) | Tripole Index for the Interdecadal Pacific Oscillation Details and more information are available. |
| NOI | Northern Oscillation Index is an index of climate variability based on the difference in SLP anomalies at the North Pacific High and near Darwin Australia. Schwing, F.B., T. Murphree, and P.M. Green. 2002. The Northern Oscillation Index (NOI): a new climate index for the northeast Pacific. Progress in Oceanography 53: 115-139. The time series and more information are available. |
| NP | North Pacific pattern is the
area-weighted sea level pressure over the region 30N-65N,
160E-140W. Time
series source Trenberth and Hurrell (1994): Climate Dynamics 9:303-319. |
| TNI (Trans-Niño Index) | Indices of El Niño evolution: Kevin E. Trenberth and
David P. Stepaniak: J. Climate, 14, 1697-1701. calculated at PSL. for longer timeseries, go to http://psl.noaa.gov/Pressure/Timeseries/TNI/ |
| Trend | A linear time series (1,2,3,...). NOT the linear trend of the variable |
| Hurricane activity | (Updated to 2016) Monthly totals Atlantic hurricanes and named tropical storms Each month has the total number of hurricanes or named tropical storms in that month in the Atlantic region. These are provided by Phil Klotabach at CSU. |
| AO | Note, values are now from CPC as they update their data
through the present
From CPC: The loading pattern of AO (AAO) is defined as the first leading mode from the EOF analysis of monthly mean height anomalies at 1000-hPa (NH) or 700-hPa (SH). Note that year-round monthly mean anomaly data has been used to obtain the loading patterns. Since the AO and AAO have the largest variability during the cold sesaon (variance of AO/AAO), the loading patterns primarily capture characteristics of the cold season patterns. Daily and monthly AO (AAO) indices are constructed by projecting the daily and monthly mean 1000-hPa (700-hPa) height anomalies onto the leading EOF mode. Both time series are normalized by the standard deviation of the monthly index (1979-2000 base period). Since the loading pattern of AO (AAO) is obtained using the monthly mean height anomaly dataset, the index corresponding to each loading pattern becomes one when it is normalized by the standard deviation of the monthly index.Values and description |
| AAO | Antarctic Oscillation. |
| Pacific Warmpool | 1st EOF of SST
(60e-170E, 15S-15N) SST EOF, all months
GISST 1948-1949
Reference:
Matin P. Hoerling (personal communication)
Reconstructed Reynolds 1950-1981 OI 1982-present |
| Tropical Pacific SST EOF | 1st EOF of SST
20N-20S, 120E-60W
GISST 1948-1949
Reference:
Martin P. Hoerling, Arun Kumar, and Taiyi Xu, 2001: Robustness of the nonlinear
climate response to ENSO's extreme phases. Journal of Climate, Vol.14, No.6,
1277-1293Reconstructed Reynolds 1950-1981 OI 1982-present |
| Atlantic Tripole SST EOF | 1st EOF of SST
10N-70N, 0-80W
GISST 1948-1949
Deser, Clara, Michael S. Timlin, 1997: Atmosphere-Ocean Interaction on Weekly Timescales in the North
Atlantic and Pacific. Journal of Climate: Vol. 10, No. 3, pp.393-408.
Reconstructed Reynolds 1950-1981 OI 1982-present |
| Atlantic multidecadal Oscillation Long Version | AMO, unsmoothed
Note: this index is newly computed from a new dataset. Please use it and note that it supersedes the old indices. The data is calculated
from the Kalplan SST. See the AMO webpage for more details.
Enfield, D.B., A. M. Mestas-Nunez and P.J. Trimble, 2001: The Atlantic multidecadal oscillation and it's
relation to rainfall and river flows in the continental U.S.. Geophysical Research Letters, Vol. 28, 2077-2080.
|
| Atlantic Meridional Mode | AMM
Note: this index is computed from a new dataset. See the AMM webpage for more details.
2004 Chiang, J. C. H., and D. J. Vimont: Analogous meridional modes of atmosphere-ocean variability in the tropical Pacific and tropical Atlantic. J. Climate,17(21), 4143-4158.
|
| North Tropical Atlantic Index (NTA) | NTA:North Tropical Atlantic SST Index
(Source dataset changed: old version available).The timeseries of SST anomalies averaged over 60W to 20W, 6N to 18N and 20W to 10W, 6N to 10N map. Data is obtained from the ERSST V3b dataset. Anomalies were calculated relative to the 1981-2010 climatology, smoothed by three months running mean procedure and projected onto 20 leading EOFs. Month of data is the center of the 3 months that are smoothed. More information and the indexes forecasted values are available.
Penland, C., and L. Matrosova, 1998: "Prediction of tropical Atlantic sea surface temperatures using Linear Inverse Modeling," J. Climate, March, 483-496 pp.
|
| Caribbean Index (CAR) | CAR:Caribbean SST Index
The timeseries of SST anomalies averaged over the the Caribbean. Data is obtained from the NOAA ERSST V3b dataset. Anomalies were calculated relative to the 1981-2010 climatology, smoothed by three months running mean procedure and projected onto 20 leading EOFs. More information and the indexes forecasted values are available.
Penland, C., and L. Matrosova, 1998: "Prediction of tropical Atlantic sea surface temperatures using Linear Inverse Modeling," J. Climate, March, 483-496 pp.
|
| Atlantic multidecadal Oscillation Long Version | AMO, smoothed
Note: this index is newly computed from a new dataset. Please use it and note that it supersedes the old indices. The data is calculated
from the Kalplan SST. See the AMO webpage for more details.
Enfield, D.B., A. M. Mestas-Nunez and P.J. Trimble, 2001: The Atlantic multidecadal oscillation and it's
relation to rainfall and river flows in the continental U.S.. Geophysical Research Letters, Vol. 28, 2077-2080.
|
| QBO | Quasi-Biennial Oscillation*. Calculated at PSL (from the zonal average of the 30mb zonal wind at the equator as computed from the NCEP/NCAR Reanalysis). |
| Globally Integrated Angular Momentum | Globally Integrated Angular Momentum*
Data is not being updated after Feb 2014. It is not known when or if it will be updated (due to resource issues)..Note that time series is scaled by 1e25. Values are 3-month running means except for the last month which is a 2-month average.
Weickmann, K.M., W.A. Robinson and M.C. Penland, 2000: Stochastic and
oscillatory forcing of global atmospheric angular momentum. J. Geophys. Res.,
105, D12, 15543-15557. |
| ENSO precipitation index | ENSO precipitation index
http://precip.gsfc.nasa.gov/ESPItable.html Please cite "ENSO Indices Based on Patterns
of Satellite-Derived Precipitation" Curtis and Adler in J. of Climate, 13,2786 (2000). Time series that uses rainfall data in the
Tropical Pacific to describe ENSO events.
|
| Central Indian Precipitation (core monsoon region) | Central Indian Precipitation
http://www.tropmet.res.in/ Please cite the Indian Institute of Tropical Meteorology.
CORE-MONSOON INDIA RAINFALL (1871-1999) 7 SUB 776,942 SQ.KM.
|
| Sahel rainfall | Sahel Standardized Rainfall (20-8N, 20W-10E)
http://jisao.washington.edu/data_sets/sahel/ From Mitchell:
The averaging region is based on the rotated principal component analysis of average June through September African rainfall presented
in Janowiak (1988, J. Climate, 1, 240-255). Stations within 20-8N, 20W-10E are obtained from the National Center for Atmospheric
Research World Monthly Surface Station Climatology (WMSSC), and 14 retained which had complete or almost complete records for
1950-93. See link for stations.
|
| SW Monsoon Region rainfall | rea averaged precipitation for Arizona and New Mexico
Calculated using NCDC's climate division dataset. Monthly precipitation values for each of the climate divisions in Arizona and New
Mexico are are averaged to produce a single monthly value. Reference:
personal communication, Catherine Smith. Also,
NCDC, 1994, Time Bias Corrected Divisional Temperature-Precipitation-Drought Index. Documentation for dataset TD-9640. Available from DBMB, NCDC, NOAA, Federal Building, 37 Battery Park Ave. Asheville, NC 28801-2733. 12pp. |
| Northeast Brazil Rainfall Anomaly | Northeast Brazil Rainfall Anomaly
http://jisao.washington.edu/data_sets/brazil/
From Mitchell: The northeast Brazil rainfall index is calculated from data for Fortaleza (3.7S, 38.5W) and Quixeramobim
(5.3S, 39.3W) Brazil obtained from the NCAR World Monthly Surface Station Climatology. Climatological mean is for 1950-79.
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| Solar Flux (10.7cm) | Solar Flux (10.7cm)*Please reacquire if you obtained it between Oct 2014 and Nov 5th 2014 as there was an error in the source data.
ftp://ftp.ngdc.noaa.gov/STP/space-weather/solar-data/solar-features/solar-radio/noontime-flux/penticton/penticton_observed/listings/listing_drao_noontime-flux-observed_monthly.txt For NGDC.
t To cite, "The 10.7cm Solar Flux Data are provided as a service by the National Research Council of Canada". They would appreciate a preprint
or at least a reference if you use the data (URL is http://www.spaceweather.ca/solarflux/sx-4-eng.php.
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| Global Mean Lan/Ocean Temperature Index | Global Mean Lan/Ocean Temperature
Values change over time!
Data values are from NASA/GISS. Please read and refer to this web page plus the main web page describing various temperature indices at the main NASA/GISTEMP webpage. Note, the index is an anomaly index. They have comments in the datafile and the writeup on obtaining an absolute global mean temperatures. Please reference the papers:
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The format for all time series is:
year1 yearN year1 janval febval marval aprval mayval junval julval augval sepval octval novval decval year2 janval febval marval aprval mayval junval julval augval sepval octval novval decval ... yearN janval febval marval aprval mayval junval julval augval sepval octval novval decval missing_value