Global Analysis - October 2001
Note: The data presented in this report are preliminary. Ranks and anomalies may change as more complete data are received and processed. Effective September 2012, the GHCN-M version 3.2.0 dataset of monthly mean temperature replaced the GHCN-M version 3.1.0 monthly mean temperature dataset. Beginning with the August 2012 Global monthly State of the Climate Report, released on September 17, 2012, GHCN-M version 3.2.0 is used for NCDC climate monitoring activities, including calculation of global land surface temperature anomalies and trends. For more information about this newest version, please see the GHCN-M version 3.2.0 Technical Report.
*The GHCN-M version 3.1.0 Technical Report was revised on September 5, 2012 to accurately reflect the changes incorporated in that version. Previously that report incorrectly included discussion of changes to the Pairwise Homogeneity Algorithm (PHA). Changes to the PHA are included in version 3.2.0 and described in the version 3.2.0 Technical Report. Please see the Frequently Asked Questions to learn more about this update.
Global Highlights:
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Contents of this Section: |
Introduction
| Anomalous warmth (using a 1992-2001 base period as shown in the adjacent blended product of satellite and in-situ data) was notable across Europe and north Africa as well as eastern Asia. While strong upper level ridges of high pressure controlled the weather in these areas during October, upper level troughs of low pressure (depicted by negative 500 millibar height anomalies) were situated across central Russia, west of the British Isles and across much of Alaska and southern Canada. Temperature anomalies calculated from in-situ station data using a 1961-1990 base period also show the cooler than average temperatures in these regions as well as over Australia. | ![]() larger image |

Temperature
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Precipitation
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References:
Peterson, T.C. and R.S. Vose, 1997: An Overview of the Global
Historical Climatology Network Database. Bull. Amer. Meteorol.
Soc., 78, 2837-2849.



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