Global temperature record
The global temperature record shows the fluctuations of the temperature of the atmosphere and the oceans through various spans of time. The most detailed information exists since 1850, when methodical thermometer-based records began. There are numerous estimates of temperatures since the end of the Pleistocene glaciation , particularly during the current Holocene epoch. Older time periods are studied by paleoclimatology .
Page Revisions
| Year | Metadata | Sections | Top Words | First Paragraph |
| 2018 |
74784 characters 10 sections 15 paragraphs 11 images 234 internal links 22 external links |
1. Satellite and balloon (1950s-present) 2. Thermometers (1850-present) 3. Tree rings and ice cores (from 1,000-2,000 years before present) 4. Paleoclimate (from 12,000 years before present) 5. Ice cores (from 800,000 years before present) |
reconstructions 0.283 rss 0.277 proxies 0.206 records 0.177 troposphere 0.170 cores 0.140 dataset 0.138 deepening 0.138 methodical 0.138 thermometer 0.138 uah 0.138 widths 0.138 infer 0.133 1978 0.133 kyr 0.133 |
The global temperature record shows the fluctuations of the temperature of the atmosphere and the oceans through various spans of time. The most detailed information exists since 1850, when methodical thermometer-based records began. There are numerous estimates of temperatures since the end of the Pleistocene glaciation , particularly during the current Holocene epoch. Older time periods are studied by paleoclimatology . |
| 2017 |
74219 characters 10 sections 15 paragraphs 11 images 234 internal links 20 external links |
1. Satellite and balloon (1950s-present) 2. Thermometers (1850-present) 3. Tree rings and ice cores (from 1,000-2,000 years before present) 4. Paleoclimate (from 12,000 years before present) 5. Ice cores (from 800,000 years before present) |
reconstructions 0.283 rss 0.277 proxies 0.206 records 0.177 troposphere 0.170 cores 0.140 dataset 0.138 deepening 0.138 methodical 0.138 thermometer 0.138 uah 0.138 widths 0.138 infer 0.133 1978 0.133 kyr 0.133 |
The global temperature record shows the fluctuations of the temperature of the atmosphere and the oceans through various spans of time. The most detailed information exists since 1850, when methodical thermometer-based records began. There are numerous estimates of temperatures since the end of the Pleistocene glaciation , particularly during the current Holocene epoch. Older time periods are studied by paleoclimatology . |
| 2016 |
72848 characters 9 sections 15 paragraphs 11 images 233 internal links 20 external links |
1. Satellite and balloon (1950s-present) 2. Thermometers (1850-present) 3. Tree rings and ice cores (from 1,000-2,000 years before present) 4. Paleoclimate (from 12,000 years before present) 5. Ice cores (from 800,000 years before present) |
reconstructions 0.283 rss 0.277 proxies 0.206 records 0.177 troposphere 0.170 cores 0.140 dataset 0.138 deepening 0.138 methodical 0.138 thermometer 0.138 uah 0.138 widths 0.138 infer 0.133 1978 0.133 kyr 0.133 |
The temperature record shows the fluctuations of the temperature of the atmosphere and the oceans through various spans of time. The most detailed information exists since 1850, when methodical thermometer-based records began. There are numerous estimates of temperatures since the end of the Pleistocene glaciation , particularly during the current Holocene epoch. Older time periods are studied by paleoclimatology . |
| 2015 |
72338 characters 9 sections 15 paragraphs 11 images 227 internal links 19 external links |
1. The Instrumental Period: from 1850 2. Tropospheric temperature (the satellite and balloon temperature records) 3. Proxies: tree rings, ice cores: the last 2000 years 5. The long term ice core record: the last 800,000 years |
reconstructions 0.288 rss 0.281 proxies 0.210 records 0.180 troposphere 0.173 cores 0.143 dataset 0.141 deepening 0.141 methodical 0.141 thermometer 0.141 uah 0.141 widths 0.141 1978 0.135 kyr 0.135 fluctuations 0.122 |
The temperature record shows the fluctuations of the temperature of the atmosphere and the oceans through various spans of time. The most detailed information exists since 1850, when methodical thermometer-based records began. There are numerous estimates of temperatures since the end of the Pleistocene glaciation , particularly during the current Holocene epoch. Older time periods are studied by paleoclimatology . |
| 2014 |
67911 characters 9 sections 15 paragraphs 11 images 225 internal links 15 external links |
1. The Instrumental Period: from 1850 2. Tropospheric temperature (the satellite and balloon temperature records) 3. Proxies: tree rings, ice cores: the last 2000 years 5. The long term ice core record: the last 800,000 years |
reconstructions 0.288 rss 0.281 proxies 0.210 records 0.180 troposphere 0.173 cores 0.143 dataset 0.141 deepening 0.141 methodical 0.141 thermometer 0.141 uah 0.141 widths 0.141 1978 0.135 kyr 0.135 fluctuations 0.122 |
The temperature record shows the fluctuations of the temperature of the atmosphere and the oceans through various spans of time. The most detailed information exists since 1850, when methodical thermometer-based records began. There are numerous estimates of temperatures since the end of the Pleistocene glaciation , particularly during the current Holocene epoch. Older time periods are studied by paleoclimatology . |
| 2013 |
67514 characters 9 sections 15 paragraphs 11 images 225 internal links 15 external links |
1. The Instrumental Period: from 1850 2. Tropospheric temperature (the satellite and balloon temperature records) 3. Proxies: tree rings, ice cores: the last 2000 years 5. The long term ice core record: the last 800,000 years |
reconstructions 0.288 rss 0.281 proxies 0.210 records 0.180 troposphere 0.173 cores 0.143 dataset 0.141 deepening 0.141 methodical 0.141 thermometer 0.141 uah 0.141 widths 0.141 1978 0.135 kyr 0.135 fluctuations 0.122 |
The temperature record shows the fluctuations of the temperature of the atmosphere and the oceans through various spans of time. The most detailed information exists since 1850, when methodical thermometer-based records began. There are numerous estimates of temperatures since the end of the Pleistocene glaciation , particularly during the current Holocene epoch. Older time periods are studied by paleoclimatology . |
| 2012 |
67514 characters 9 sections 15 paragraphs 11 images 225 internal links 15 external links |
1. The Instrumental Period: from 1850 2. Tropospheric temperature (the satellite and balloon temperature records) 3. Proxies: tree rings, ice cores: the last 2000 years 5. The long term ice core record: the last 800,000 years |
reconstructions 0.288 rss 0.281 proxies 0.210 records 0.180 troposphere 0.173 cores 0.143 dataset 0.141 deepening 0.141 methodical 0.141 thermometer 0.141 uah 0.141 widths 0.141 1978 0.135 kyr 0.135 fluctuations 0.122 |
The temperature record shows the fluctuations of the temperature of the atmosphere and the oceans through various spans of time. The most detailed information exists since 1850, when methodical thermometer-based records began. There are numerous estimates of temperatures since the end of the Pleistocene glaciation , particularly during the current Holocene epoch. Older time periods are studied by paleoclimatology . |
| 2011 |
67553 characters 9 sections 15 paragraphs 11 images 225 internal links 14 external links |
1. The Instrumental Period: from 1850 2. Tropospheric temperature (the satellite and balloon temperature records) 3. Proxies: tree rings, ice cores: the last 2000 years 5. The long term ice core record: the last 800,000 years |
reconstructions 0.288 rss 0.281 proxies 0.210 records 0.180 troposphere 0.173 cores 0.143 dataset 0.141 deepening 0.141 methodical 0.141 thermometer 0.141 uah 0.141 widths 0.141 1978 0.135 kyr 0.135 fluctuations 0.122 |
The temperature record shows the fluctuations of the temperature of the atmosphere and the oceans through various spans of time. The most detailed information exists since 1850, when methodical thermometer-based records began. There are numerous estimates of temperatures since the end of the Pleistocene glaciation , particularly during the current Holocene epoch. Older time periods are studied by paleoclimatology . |
| 2010 |
59494 characters 9 sections 13 paragraphs 10 images 224 internal links 9 external links |
1. The Instrumental Period: from 1850 2. Tropospheric temperature (the satellite and balloon temperature records) 3. Proxies: tree rings, ice cores: the last 2000 years 5. The long term ice core record: the last 800,000 years |
reconstructions 0.295 rss 0.288 proxies 0.215 records 0.184 cores 0.146 deepening 0.144 methodical 0.144 thermometer 0.144 uah 0.144 widths 0.144 kyr 0.139 fluctuations 0.125 troposphere 0.118 epica 0.118 proxy 0.110 |
The temperature record shows the fluctuations of the temperature of the atmosphere and the oceans through various spans of time. The most detailed information exists since 1850, when methodical thermometer-based records began. There are numerous estimates of temperatures since the end of the Pleistocene glaciation , particularly during the current Holocene epoch. Older time periods are studied by paleoclimatology . |
| 2009 |
55218 characters 9 sections 11 paragraphs 10 images 218 internal links 9 external links |
1. The Instrumental Period: from 1850 2. Tropospheric temperature (the satellite and balloon temperature records) 3. Proxies: tree rings, ice cores: the last 2000 years 5. The long term ice core record: the last 800,000 years |
rss 0.334 proxies 0.207 records 0.189 deepening 0.167 methodical 0.167 thermometer 0.167 uah 0.167 widths 0.167 troposphere 0.137 epica 0.137 numerical 0.137 ring 0.124 epoch 0.119 pleistocene 0.119 connecting 0.119 |
The temperature record shows the fluctuations of the temperature of the atmosphere and the oceans through various spans of time. The most detailed information exists since 1850, when methodical thermometer-based records began. There are numerous estimates of temperatures since the end of the Pleistocene glaciation , particularly during the current Holocene epoch. Older time periods are studied by paleoclimatology . |
| 2008 |
54318 characters 9 sections 11 paragraphs 10 images 215 internal links 9 external links |
1. The Instrumental Period: from 1850 2. Tropospheric temperature (the satellite and balloon temperature records) 3. Proxies: tree rings, ice cores: the last 2000 years 5. The long term ice core record: the last 800,000 years |
proxies 0.224 records 0.204 deepening 0.180 methodical 0.180 rss 0.180 thermometer 0.180 widths 0.180 troposphere 0.148 epica 0.148 numerical 0.148 ring 0.134 epoch 0.129 pleistocene 0.129 connecting 0.129 kyr 0.116 |
The temperature record shows the fluctuations of the temperature of the atmosphere and the oceans through various spans of time. The most detailed information exists since 1850, when methodical thermometer-based records began. There are numerous estimates of temperatures since the end of the Pleistocene glaciation , particularly during the current Holocene epoch. Older time periods are studied by paleoclimatology . |
| 2007 |
53662 characters 8 sections 10 paragraphs 9 images 216 internal links 9 external links |
1. The Instrumental Period: from 1850 2. Tropospheric temperature (the satellite and balloon temperature records) 3. Proxies: tree rings, ice cores: the last 2000 years 5. The long term ice core record: the last 800,000 years |
proxies 0.224 records 0.205 deepening 0.180 methodical 0.180 rss 0.180 thermometer 0.180 widths 0.180 troposphere 0.148 epica 0.148 numerical 0.148 ring 0.134 epoch 0.129 pleistocene 0.129 connecting 0.129 kyr 0.116 |
The temperature record shows the fluctuations of the temperature of the atmosphere and the oceans through various spans of time. The most detailed information exists since 1850 , when methodical thermometer-based records began. There are numerous estimates of temperatures since the end of the Pleistocene glaciation , particularly during the current Holocene epoch. Older time periods are studied by paleoclimatology . |
| 2006 |
52353 characters 8 sections 10 paragraphs 9 images 211 internal links 9 external links |
1. The Instrumental Period: from 1850 2. Tropospheric temperature (the satellite and balloon temperature records) 3. Proxies: tree rings, ice cores: the last 2000 years 5. The long term ice core record: the last 800,000 years |
proxies 0.224 records 0.205 deepening 0.180 methodical 0.180 rss 0.180 thermometer 0.180 widths 0.180 troposphere 0.148 epica 0.148 numerical 0.148 ring 0.134 epoch 0.129 pleistocene 0.129 connecting 0.129 kyr 0.116 |
The temperature record shows the fluctuations of the temperature of the atmosphere and the oceans through various spans of time. The most detailed information exists since 1850 , when methodical thermometer-based records began. There are numerous estimates of temperatures since the end of the Pleistocene glaciation , particularly during the current Holocene epoch. Older time periods are studied by paleoclimatology . |
| 2005 |
19142 characters 8 sections 10 paragraphs 6 images 26 internal links 8 external links |
1. The Instrumental Period: from 1850 2. Tropospheric temperature (the satellite and balloon temperature records) 3. Proxies: tree rings, ice cores: the last 2000 years 5. The long term ice core record: the last 800,000 years |
proxies 0.225 records 0.205 deepening 0.181 methodical 0.181 rss 0.181 thermometer 0.181 widths 0.181 troposphere 0.149 epica 0.149 numerical 0.149 ring 0.135 epoch 0.130 pleistocene 0.130 connecting 0.130 kyr 0.116 |
The temperature record shows the fluctuations of the temperature of the atmosphere and the oceans through various spans of time. The most detailed information exists since 1850 , when methodical thermometer-based records began. There are numerous estimates of temperatures since the end of the Pleistocene glaciation , particularly during the current Holocene epoch. Older time periods are studied by paleoclimatology . |