Wskaźnik mTPI odróżnia grzbiety od dolin. Jest on obliczany na podstawie danych o wysokości nad poziomem morza w każdej lokalizacji, od których odejmowana jest średnia wysokość nad poziomem morza w danej okolicy. mTPI wykorzystuje ruchome okna o promieniach (w km): 115,8, 89,9, 35,5, 13,1, 5,6, 2,8 i 1,2. Jest on oparty na modelu DEM SRTM o rozdzielczości 30 m (dostępnym w EE jako USGS/SRTMGL1_003).
Zbiory danych Conservation Science Partners (CSP) Ecologically Relevant Geomorphology (ERGo), Landforms and Physiography zawierają szczegółowe dane wieloskalowe dotyczące form terenu i wzorców fizjograficznych (czyli aspektów terenu). Chociaż dane te można wykorzystać na wiele sposobów, ich pierwotnym celem było opracowanie istotnej z ekologicznego punktu widzenia klasyfikacji i mapy form terenu oraz klas fizjograficznych, które nadają się do planowania adaptacji do zmian klimatu. Przyszłe warunki klimatyczne są obarczone dużą niepewnością, a reakcje ekologiczne są jeszcze bardziej niepewne. Dlatego informacje o tym, co prawdopodobnie się nie zmieni, stanowią solidną podstawę do opracowywania przez menedżerów solidnych planów adaptacji do zmian klimatu. Kwantyfikacja tych cech krajobrazu jest wrażliwa na rozdzielczość, dlatego podajemy najwyższą możliwą rozdzielczość, biorąc pod uwagę zakres i charakterystykę danego indeksu.
Pasma
Rozmiar piksela 270 metrów
Pasma
Nazwa
Jednostki
Minimum
Maks.
Rozmiar piksela
Opis
elevation
m
-8129*
7905*
metry
Wartości mTPI pochodzące z danych SRTM, od ujemnych (doliny) do dodatnich (grzbiety)
Theobald, D. M., Harrison-Atlas, D., Monahan, W. B., & Albano, C. M.
(2015). Mapy form terenu i różnorodności fizjograficznej istotne z ekologicznego punktu widzenia na potrzeby planowania adaptacji do zmian klimatu. PloS one, 10(12),
e0143619
Wskaźnik mTPI odróżnia grzbiety od dolin. Jest on obliczany na podstawie danych o wysokości nad poziomem morza w każdej lokalizacji, od których odejmowana jest średnia wysokość nad poziomem morza w danej okolicy. W przypadku mTPI stosowane są ruchome okna o promieniach (w km): 115,8, 89,9, 35,5, 13,1, 5,6, 2,8 i 1,2. Jest on oparty na modelu DEM SRTM o rozdzielczości 30 m (dostępnym w EE…
[null,null,[],[[["\u003cp\u003eThe Conservation Science Partners (CSP) Ecologically Relevant Geomorphology (ERGo) dataset provides multi-scale data on landforms and physiographic patterns for climate adaptation planning.\u003c/p\u003e\n"],["\u003cp\u003eThe dataset features a global SRTM-derived mTPI (Multi-Scale Topographic Position Index) at a 270-meter resolution, distinguishing ridge from valley forms based on elevation data.\u003c/p\u003e\n"],["\u003cp\u003eThe mTPI is calculated using moving windows of radius (km): 115.8, 89.9, 35.5, 13.1, 5.6, 2.8, and 1.2, and is based on the 30m SRTM DEM.\u003c/p\u003e\n"],["\u003cp\u003eThe dataset is available from January 24, 2006 to May 13, 2011 and is licensed under CC-BY-NC-SA-4.0.\u003c/p\u003e\n"]]],["The dataset, provided by Conservation Science Partners, covers 2006-01-24 to 2011-05-13. It features the multi-scale Topographic Position Index (mTPI), which differentiates ridges from valleys using elevation data. Calculated by subtracting each location's elevation from the mean neighborhood elevation. The mTPI uses various moving window radii and is derived from 30m SRTM DEM data, and provides multi-scale landform and physiographic data for climate adaptation planning. Data is available via Earth Engine.\n"],null,["# Global SRTM mTPI (Multi-Scale Topographic Position Index)\n\nDataset Availability\n: 2006-01-24T00:00:00Z--2011-05-13T00:00:00Z\n\nDataset Provider\n:\n\n\n [Conservation Science Partners](https://www.csp-inc.org/)\n\nTags\n:\n[aspect](/earth-engine/datasets/tags/aspect) [csp](/earth-engine/datasets/tags/csp) [elevation](/earth-engine/datasets/tags/elevation) [elevation-topography](/earth-engine/datasets/tags/elevation-topography) [ergo](/earth-engine/datasets/tags/ergo) [geophysical](/earth-engine/datasets/tags/geophysical) [global](/earth-engine/datasets/tags/global) [landforms](/earth-engine/datasets/tags/landforms) [slope](/earth-engine/datasets/tags/slope) [topography](/earth-engine/datasets/tags/topography) \n\n#### Description\n\nThe mTPI distinguishes ridge from valley forms. It is calculated using\nelevation data for each location subtracted by the mean elevation within a\nneighborhood. mTPI uses moving windows of radius (km): 115.8, 89.9, 35.5,\n13.1, 5.6, 2.8, and 1.2. It is based on the 30m SRTM DEM (available in EE\nas USGS/SRTMGL1_003).\n\nThe Conservation Science Partners (CSP) Ecologically Relevant Geomorphology\n(ERGo) Datasets, Landforms and Physiography contain detailed, multi-scale\ndata on landforms and physiographic (aka land facet) patterns. Although\nthere are many potential uses of these data, the original purpose for these\ndata was to develop an ecologically relevant classification and map of\nlandforms and physiographic classes that are suitable for climate adaptation\nplanning. Because there is large uncertainty associated with future climate\nconditions and even more uncertainty around ecological responses, providing\ninformation about what is unlikely to change offers a strong foundation for\nmanagers to build robust climate adaptation plans. The quantification of\nthese features of the landscape is sensitive to the resolution, so we\nprovide the highest resolution possible given the extent and characteristics\nof a given index.\n\n### Bands\n\n\n**Pixel Size**\n\n270 meters\n\n**Bands**\n\n| Name | Units | Min | Max | Pixel Size | Description |\n|-------------|-------|---------|--------|------------|-------------------------------------------------------------------------------|\n| `elevation` | m | -8129\\* | 7905\\* | meters | SRTM-derived mTPI ranging from negative (valleys) to positive (ridges) values |\n\n\\* estimated min or max value\n\n### Terms of Use\n\n**Terms of Use**\n\n[CC-BY-NC-SA-4.0](https://spdx.org/licenses/CC-BY-NC-SA-4.0.html)\n\n### Citations\n\nCitations:\n\n- Theobald, D. M., Harrison-Atlas, D., Monahan, W. B., \\& Albano, C. M.\n (2015). Ecologically-relevant maps of landforms and physiographic diversity\n for climate adaptation planning. PloS one, 10(12),\n [e0143619](https://journals.plos.org/plosone/article?id=10.1371/journal.pone.0143619)\n\n### Explore with Earth Engine\n\n| **Important:** Earth Engine is a platform for petabyte-scale scientific analysis and visualization of geospatial datasets, both for public benefit and for business and government users. Earth Engine is free to use for research, education, and nonprofit use. To get started, please [register for Earth Engine access.](https://console.cloud.google.com/earth-engine)\n\n### Code Editor (JavaScript)\n\n```javascript\nvar dataset = ee.Image('CSP/ERGo/1_0/Global/SRTM_mTPI');\nvar srtmMtpi = dataset.select('elevation');\nvar srtmMtpiVis = {\n min: -200.0,\n max: 200.0,\n palette: ['0b1eff', '4be450', 'fffca4', 'ffa011', 'ff0000'],\n};\nMap.setCenter(-105.8636, 40.3439, 11);\nMap.addLayer(srtmMtpi, srtmMtpiVis, 'SRTM mTPI');\n```\n[Open in Code Editor](https://code.earthengine.google.com/?scriptPath=Examples:Datasets/CSP/CSP_ERGo_1_0_Global_SRTM_mTPI) \n[Global SRTM mTPI (Multi-Scale Topographic Position Index)](/earth-engine/datasets/catalog/CSP_ERGo_1_0_Global_SRTM_mTPI) \nThe mTPI distinguishes ridge from valley forms. It is calculated using elevation data for each location subtracted by the mean elevation within a neighborhood. mTPI uses moving windows of radius (km): 115.8, 89.9, 35.5, 13.1, 5.6, 2.8, and 1.2. It is based on the 30m SRTM DEM (available in EE ... \nCSP/ERGo/1_0/Global/SRTM_mTPI, aspect,csp,elevation,elevation-topography,ergo,geophysical,global,landforms,slope,topography \n2006-01-24T00:00:00Z/2011-05-13T00:00:00Z \n-90 -180 90 180 \nGoogle Earth Engine \nhttps://developers.google.com/earth-engine/datasets\n\n- [](https://doi.org/https://www.csp-inc.org/)\n- [](https://doi.org/https://developers.google.com/earth-engine/datasets/catalog/CSP_ERGo_1_0_Global_SRTM_mTPI)"]]
