data: $partialdiff sub T$ [ NOAA NCEP CPC Indices NHTI EA ]

served from IRI/LDEO Climate Data Library

∂_T [ NOAA NCEP CPC Indices NHTI EA ]: ∂_T East Atlantic Pattern data

NHTI EA ∂_T East Atlantic Pattern from NOAA NCEP CPC Indices: Northern Hemisphere Teleconnection Indices.

Independent Variables (Grids)

Time (time): grid: /T (months since 1960-01-01) ordered (16 Jan 1950 - 15 Feb 1950) to (16 Mar 2024 - 15 Apr 2024) by 1.0 N= 891 pts :grid

Other Info

file_missing_value: -99.900002
missing_value: NaN
units: 12 year^-1

References

Barnston, A. G., and R. E. Livezey, 1987: Classification, seasonality and persistence of low-frequency atmospheric circulation patterns. Mon. Wea. Rev., 115, 1083-1126.

Bell, G. D., and M. S. Halpert, 1995: Atlas of intraseasonal and interannual variability, 1986-1993. NOAA Atlas No. 12. Climate Prediction Center, NOAA/NWS/NMC, Washington D.C.

Hurrell, J. W., 1995: Decadal trends in the North Atlantic Oscillation: Regional temperatures and precipitation. Science, 269, 676-679.

Mo, K. C., and R. E. Livezey, 1986: Tropical-extratropical geopotential height teleconnections during the Northern Hemisphere winter. Mon. Wea. Rev., 114, 2488-2515.

Wallace, J. M., and D. S. Gutzler, 1981: Teleconnections in the geopotential height field during the Northern Hemisphere winter. Mon. Wea. Rev., 109, 784-812.

Last updated: Sun, 05 May 2024 05:03:46 GMT
Expires: Tue, 04 Jun 2024 00:00:00 GMT

Data Views

	T
$partialdiff sub T$ [ NOAA NCEP CPC Indices NHTI EA ][ T \|]	M

Filters

Here are some filters that are useful for manipulating data. There are actually many more available, but they have to be entered manually. See Ingrid Function Documentation for more information.

Monthly Climatology calculates a monthly climatology by averaging over all years.
anomalies calculates the difference between the (above) monthly climatology and the original data.
Integrate along T
Differentiate along T
Take differences along T