Hayashi, T (1997): Component parts of the World Heat Flow Data Collection [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.809754
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Source:
International Heat Flow Commission, I H F C (2012): Global Heat Flow Database. The Global Heat Flow Database of the International Heat Flow Commission (IHFC), University of North Dakota, USA; (data copied, 2012-10), https://ihfc-iugg.org/products/global-heat-flow-database/data
Further details:
Jessop, Alan M; Hobart, Michael A; Sclater, John G (1976): The World Heat Flow Data Collection - 1975. Geological Survey of Canada, Earth Physics Branch, Geothermal Series, 5, 10 pp, hdl:10013/epic.40176.d002
Coverage:
Median Latitude: 53.559042 * Median Longitude: 146.813192 * South-bound Latitude: 52.961700 * West-bound Longitude: 146.028300 * North-bound Latitude: 54.586700 * East-bound Longitude: 148.098300
Minimum ELEVATION: -1750 m a.s.l. * Maximum ELEVATION: -1210 m a.s.l.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Area/locality | Area | Hayashi, T | |||
2 | Sample, optional label/labor no | Lab no | Hayashi, T | |||
3 | LATITUDE | Latitude | Geocode | |||
4 | LONGITUDE | Longitude | Geocode | |||
5 | ELEVATION | Elevation | m a.s.l. | Geocode | ||
6 | Depth, bottom/max | Depth bot | m | Hayashi, T | Maximum depth | |
7 | Number of temperature data | No Temps | Hayashi, T | |||
8 | Temperature gradient | T grad | mK/m | Hayashi, T | ||
9 | Number of conductivity measurements | No Cond | Hayashi, T | |||
10 | Conductivity, average | Cond average | W/m K | Hayashi, T | ||
11 | Heat flow | HF | mW/m2 | Hayashi, T |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
189 data points
Data
1 Area | 2 Lab no | 3 Latitude | 4 Longitude | 5 Elevation [m a.s.l.] | 6 Depth bot [m] | 7 No Temps | 8 T grad [mK/m] | 9 No Cond | 10 Cond average [W/m K] | 11 HF [mW/m2] |
---|---|---|---|---|---|---|---|---|---|---|
Sea of Okhotsk | OKHHF01B | 53.0317 | 146.0900 | -1750 | 4 | 6 | 84 | 0.72 | 61 | |
Sea of Okhotsk | OKHHF01C | 53.0350 | 146.0917 | -1750 | 3 | 5 | 89 | 0.72 | 64 | |
Sea of Okhotsk | OKHHF03B | 53.0517 | 146.5717 | -1670 | 3 | 6 | 113 | 0.70 | 79 | |
Sea of Okhotsk | OKHHF04B | 53.1167 | 146.8133 | -1720 | 4 | 7 | 95 | 2 | 0.76 | 72 |
Sea of Okhotsk | OKHHF05A | 53.2533 | 146.0283 | -1490 | 4 | 7 | 82 | 2 | 0.79 | 65 |
Sea of Okhotsk | OKHHF05B | 53.2567 | 147.0300 | -1490 | 4 | 7 | 85 | 2 | 0.83 | 70 |
Sea of Okhotsk | OKHHF05D | 53.2600 | 147.0333 | -1490 | 3 | 6 | 100 | 2 | 0.85 | 85 |
Sea of Okhotsk | OKHHF06A | 53.1067 | 147.4183 | -1460 | 3 | 7 | 87 | 2 | 0.84 | 73 |
Sea of Okhotsk | OKHHF06C | 53.1050 | 147.4300 | -1460 | 4 | 7 | 81 | 2 | 0.83 | 68 |
Sea of Okhotsk | OKHHF07A | 53.1183 | 147.5550 | -1470 | 4 | 7 | 81 | 2 | 0.78 | 63 |
Sea of Okhotsk | OKHHF07B | 53.1200 | 147.5517 | -1470 | 3 | 7 | 88 | 2 | 0.80 | 71 |
Sea of Okhotsk | OKHHF07C | 53.1217 | 147.5667 | -1470 | 2 | 7 | 102 | 2 | 0.76 | 78 |
Sea of Okhotsk | OKHHF08C | 52.9617 | 148.0950 | -1530 | 3 | 6 | 59 | 2 | 0.74 | 44 |
Sea of Okhotsk | OKHHF08D | 52.9617 | 148.0983 | -1530 | 3 | 6 | 68 | 2 | 0.75 | 51 |
Sea of Okhotsk | OKHHF09A | 53.8917 | 146.4150 | -1630 | 4 | 6 | 96 | 2 | 0.69 | 66 |
Sea of Okhotsk | OKHHF09B | 53.8950 | 146.4083 | -1630 | 3 | 6 | 100 | 2 | 0.81 | 81 |
Sea of Okhotsk | OKHHF10A | 54.0183 | 146.4250 | -1600 | 2 | 5 | 110 | 2 | 0.99 | 109 |
Sea of Okhotsk | OKHHF10B | 54.0200 | 146.4267 | -1600 | 3 | 6 | 164 | 2 | 0.95 | 156 |
Sea of Okhotsk | OKHHF10C | 54.0217 | 146.4250 | -1600 | 3 | 7 | 97 | 2 | 0.93 | 90 |
Sea of Okhotsk | OKHHF11A | 54.1550 | 146.4350 | -1690 | 4 | 7 | 95 | 2 | 0.79 | 74 |
Sea of Okhotsk | OKHHF11B | 54.1567 | 146.4400 | -1690 | 3 | 7 | 97 | 2 | 0.73 | 71 |
Sea of Okhotsk | OKHHF12A | 54.5850 | 146.3883 | -1210 | 3 | 7 | 91 | 2 | 0.78 | 71 |
Sea of Okhotsk | OKHHF12B | 54.5867 | 146.3900 | -1210 | 3 | 7 | 93 | 2 | 0.80 | 75 |
Sea of Okhotsk | OKHHF12C | 54.5867 | 146.3900 | -1210 | 3 | 7 | 91 | 2 | 0.79 | 72 |