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Note: The data presented in this report are preliminary. Ranks and anomalies may change as more complete data are received and processed. Effective November 2011, the GHCN-M version 3.1.0 dataset of monthly mean temperature replaced the GHCN-M version 3 monthly mean temperature dataset. Beginning with the October 2011 Global monthly State of the Climate Report, GHCN-M version 3.1.0 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 Modifications to Pairwise Homogeneity Adjustment software to address coding errors and improve run-time efficiency.
October 2011 Selected Climate
Anomalies and Events Map
Please Note: The data presented in this report are preliminary. Ranks and anomalies may change as more complete data are received and processed. Effective with the October 2009 State of the Climate Report, NCDC transitioned to the new version (version 3b) of the extended reconstructed sea surface temperature (ERSST) dataset. ERSST.v3b is an improved extended SST reconstruction over version 2. For more information about the differences between ERSST.v3b and ERSST.v2 and to access the most current data, please visit NCDC's Global Surface Temperature Anomalies page.
Temperature anomalies for October 2011 are shown on the dot maps below. The dot map on the left provides a spatial representation of anomalies calculated from the Global Historical Climatology Network (GHCN) dataset of land surface stations using a 1961–1990 base period. The dot map on the right is a product of a merged land surface and sea surface temperature (SST) anomaly analysis developed by Smith et al. (2008). For the merged land surface and SST analysis, temperature anomalies with respect to the 1971–2000 average for land and ocean are analyzed separately and then merged to form the global analysis. For more information, please visit NCDC's Global Surface Temperature Anomalies page.
October 2011 was much warmer than normal compared with previous Octobers. On average, land areas across the Northern Hemisphere—where the majority of the Earth's land mass is located—were the warmest on record for the month, at 1.29°C (2.32°F) above the 20th century average. The warmth was especially pronounced across Alaska, Canada, Mongolia, and most of Russia and Europe. According to the UK Met Office, the United Kingdom marked its warmest October since 2006 and eighth warmest in the last 100 years, at 2.0°C (3.6°F) above the 1971–2000 average. Norway also reported its eighth warmest October, at 1.8°C (2.6°F) above normal, with records dating back to 1900.The dot maps below show much of central and northern Russia with average temperatures more than 5°C (9°F) above average. Temperatures in the Southern Hemisphere were also above average, ranking 16th warmest on record. However, most of southern and western South America was cooler than average. According to the Argentina Meteorological Service (Servicio Meteorológico Nacional), several locations in Argentina experienced their coolest October in five decades. Globally, the average October land surface temperature was second warmest on record, at 1.10°C (1.98°F) above average.
La Niña conditions continued to strengthen in the eastern central Pacific Ocean during October, according to NOAA's Climate Prediction Center. Globally, the average October sea surface temperature was 13th warmest on record, with similar monthly average temperature anomalies in both the Northern and Southern Hemisphere oceans. While it was cooler than normal in the region of the Pacific where ENSO conditions are measured and also in the northeast Pacific, it was notably warmer than normal across the north central and northwest Pacific, the northeast Atlantic, and portions of the mid-latitude Southern oceans.
Overall, the combined global average land and ocean temperature ranked as the eighth warmest October in the 132-year period of record.
La Niña conditions have been present during all months to-date in 2011, with the exception of May, June, and July, when ENSO-neutral conditions briefly returned. These conditions impacted temperatures around the globe, making the January–October combined global land and ocean temperature the 10th warmest such period on record and the coolest since 2008, at 0.53°C (0.95°F) above average. The
January–October 2011 map of temperature anomalies shows regions with anomalously warm and anomalously cool temperatures. Over land, the most anomalous warmth enveloped nearly all of central and western Russia. Few regions were cooler than normal, most notably much of northern Australia the north central and northwest United States, and southwest Canada. Overall, the global land surface temperature anomaly (0.85°C / 1.53°F) was more than twice as high as the global sea surface temperature anomaly (0.41°C / 0.74°F) for this period, ranking as 6th warmest and 12th warmest, respectively.
The average position of the upper-level ridges of high pressure and troughs of low pressure (depicted by positive and negative 500-millibar height anomalies on the
October 2011 map, respectively) are generally reflected by areas of positive and negative temperature anomalies at the surface, respectively. For other Global products, please see the Climate Monitoring Global Products page.
Images of sea surface temperature anomalies are available for each week from 2004 to present on the weekly SST page.
| October | Anomaly | Rank (out of 132 years) |
Records | |||
|---|---|---|---|---|---|---|
| °C | °F | Year(s) | °C | °F | ||
| Global | ||||||
| Land | +1.10 ± 0.11 | +1.98 ± 0.20 | 2nd Warmest | Warmest: 2005 | +1.14 | +2.05 |
| 131st Coolest | Coolest: 1976 | -0.88 | -1.58 | |||
| Ocean | +0.39 ± 0.04 | +0.70 ± 0.07 | 11th Warmest | Warmest: 2003 | +0.58 | +1.04 |
| 122nd Coolest | Coolest: 1909 | -0.47 | -0.85 | |||
| Ties: 1998 | ||||||
| Land and Ocean | +0.58 ± 0.07 | +1.04 ± 0.13 | 8th Warmest | Warmest: 2003 | +0.72 | +1.30 |
| 125th Coolest | Coolest: 1912 | -0.54 | -0.97 | |||
| Northern Hemisphere | ||||||
| Land | +1.29 ± 0.11 | +2.32 ± 0.20 | 1st Warmest | Warmest: 2003 | +1.25 | +2.25 |
| 132nd Coolest | Coolest: 1912 | -1.15 | -2.07 | |||
| Ocean | +0.40 ± 0.04 | +0.72 ± 0.07 | 12th Warmest | Warmest: 2003, 2006 | +0.65 | +1.17 |
| 121st Coolest | Coolest: 1912 | -0.50 | -0.90 | |||
| Land and Ocean | +0.73 ± 0.08 | +1.31 ± 0.14 | 5th Warmest | Warmest: 2003 | +0.88 | +1.58 |
| 128th Coolest | Coolest: 1912 | -0.74 | -1.33 | |||
| Southern Hemisphere | ||||||
| Land | +0.58 ± 0.17 | +1.04 ± 0.31 | 16th Warmest | Warmest: 2006 | +1.15 | +2.07 |
| 117th Coolest | Coolest: 1910 | -0.74 | -1.33 | |||
| Ocean | +0.39 ± 0.04 | +0.70 ± 0.07 | 13th Warmest | Warmest: 1997 | +0.59 | +1.06 |
| 120th Coolest | Coolest: 1910 | -0.46 | -0.83 | |||
| Land and Ocean | +0.42 ± 0.06 | +0.76 ± 0.11 | 12th Warmest | Warmest: 1997 | +0.62 | +1.12 |
| 121st Coolest | Coolest: 1910 | -0.51 | -0.92 | |||
| Ties: 1996, 2001, 2007 | ||||||
| January–October | Anomaly | Rank (out of 132 years) |
Records | |||
|---|---|---|---|---|---|---|
| °C | °F | Year(s) | °C | °F | ||
| Global | ||||||
| Land | +0.85 ± 0.19 | +1.53 ± 0.34 | 6th Warmest | Warmest: 2007 | +1.06 | +1.91 |
| 127th Coolest | Coolest: 1893 | -0.62 | -1.12 | |||
| Ties: 2009 | ||||||
| Ocean | +0.41 ± 0.04 | +0.74 ± 0.07 | 12th Warmest | Warmest: 1998 | +0.54 | +0.97 |
| 121st Coolest | Coolest: 1911 | -0.47 | -0.85 | |||
| Land and Ocean | +0.53 ± 0.09 | +0.95 ± 0.16 | 10th Warmest | Warmest: 2010 | +0.66 | +1.19 |
| 123rd Coolest | Coolest: 1911 | -0.45 | -0.81 | |||
| Ties: 2001 | ||||||
| Northern Hemisphere | ||||||
| Land | +0.96 ± 0.20 | +1.73 ± 0.36 | 5th Warmest | Warmest: 2007 | +1.19 | +2.14 |
| 128th Coolest | Coolest: 1893 | -0.67 | -1.21 | |||
| Ocean | +0.40 ± 0.04 | +0.72 ± 0.07 | 12th Warmest | Warmest: 2005 | +0.56 | +1.01 |
| 121st Coolest | Coolest: -0.47 | -0.85 | 0.05 | |||
| Ties: 2008 | ||||||
| Land and Ocean | +0.61 ± 0.13 | +1.10 ± 0.23 | 10th Warmest | Warmest: 2010 | +0.75 | +1.35 |
| 123rd Coolest | Coolest: -0.47 | -0.85 | 0.06 | |||
| Southern Hemisphere | ||||||
| Land | +0.57 ± 0.15 | +1.03 ± 0.27 | 12th Warmest | Warmest: 2005 | +0.92 | +1.66 |
| 121st Coolest | Coolest: 1917 | -0.73 | -1.31 | |||
| Ties: 1983, 2008 | ||||||
| Ocean | +0.43 ± 0.04 | +0.77 ± 0.07 | 11th Warmest | Warmest: 1998 | +0.56 | +1.01 |
| 122nd Coolest | Coolest: 1911 | -0.51 | -0.92 | |||
| Land and Ocean | +0.45 ± 0.07 | +0.81 ± 0.13 | 12th Warmest | Warmest: 1998 | +0.62 | +1.12 |
| 121st Coolest | Coolest: 1911 | -0.52 | -0.94 | |||
The most current data may be accessed via the Global Surface Temperature Anomalies page.
The maps below represent anomaly values based on the GHCN dataset of land surface stations using a base period of 1961–1990. Precipitation anomalies on a month-to-month basis are often highly variable across the globe and even within regions.
There were several areas across the globe with anomalous wetness or anomalous dryness during October. With the end of the South Asian monsoon season, India and Bangladesh observed drier-than-normal conditions. It was also abnormally dry in northeastern China, eastern Australia, the central United States and much of Canada. An unusually wet monsoon season brought devastating floods to Thailand. Seasonal rains brought wetter-than-normal conditions to Algeria and Ethiopia. The remnants of Hurricane Rina affected south Florida and brought heavy precipitation in the form of snowfall to the northeast United States. Other regions that experienced above-average rainfall included eastern South America, the northwest United States, Western Australia, and Pakistan.
Rainfall across Australia was 52 percent above average, making this month the 17th wettest October in its 112-year period of record, according to Australia's Bureau of Meteorology. The wetness was due largely to well-above average rainfall in the tropical north and western half of the country. Western Australia saw average rainfall more than two times higher than normal, making this October its third wettest on record and wettest since 1975. Weak La Niña conditions were present in October, and La Niña is associated with heavier-than-average precipitation in Australia.
Additional details on extreme climate events and flooding and drought conditions can also be found on the October 2011 Global Hazards page.
Peterson, T.C. and R.S. Vose, 1997: An Overview of the Global Historical Climatology Network Database. Bull. Amer. Meteorol. Soc., 78, 2837-2849.
Quayle, R.G., T.C. Peterson, A.N. Basist, and C. S. Godfrey, 1999: An operational near-real-time global temperature index. Geophys. Res. Lett., 26, 333-335.
Smith, T.M., and R.W. Reynolds (2005), A global merged land air and sea surface temperature reconstruction based on historical observations (1880-1997), J. Clim., 18, 2021-2036.
Smith, et al (2008), Improvements to NOAA's Historical Merged Land-Ocean Surface Temperature Analysis (1880-2006), J. Climate., 21, 2283-2293.
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