data: $integral dT$ [ NOAA NCEP CPC Indices NHTI EAWR ]

served from IRI/LDEO Climate Data Library

∫dT [ NOAA NCEP CPC Indices NHTI EAWR ]: East Atlantic/West Russia Pattern data

NHTI EAWR East Atlantic/West Russia Pattern from NOAA NCEP CPC Indices: Northern Hemisphere Teleconnection Indices.

Independent Variables (Grids)

Time (time): grid: /T (months since 1960-01-01) ordered (0000 1 Jan 1950) to (0000 1 May 2024) by 1.0 N= 893 pts :grid

Other Info

bufferwordsize: 8
datatype: doublearraytype
file_missing_value: -99.900002
missing_value: NaN
units: months
standard units*: 0.0833333333333333 year

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
$integral dT$ [ NOAA NCEP CPC Indices NHTI EAWR ][ 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