Analysis of soil moisture patterns in forested and suburban catchments in Baltimore, Maryland, using high-resolution photogrammetric and LIDAR digital elevation datasets
Field observations of near‐surface soil moisture, collected over several seasons in a watershed in suburban Maryland, are compared with values of the topographic soil moisture index generated using digital elevation models (DEMs) at a range of grid cell sizes from photogrammetric and light detection...
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| Veröffentlicht in: | Hydrological processes 2006-02, Vol.20 (2), p.219-240 |
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| creator | Tenenbaum, D. E. Band, L. E. Kenworthy, S. T. Tague, C. L. |
| description | Field observations of near‐surface soil moisture, collected over several seasons in a watershed in suburban Maryland, are compared with values of the topographic soil moisture index generated using digital elevation models (DEMs) at a range of grid cell sizes from photogrammetric and light detection and ranging (LIDAR) data sources. A companion set of near‐surface soil moisture observations, DEMs and topographic index values are also presented for a nearby forested catchment. The degree to which topographic index values are an effective indicator of near‐surface soil moisture conditions varies in the two environments. The urbanizing environment requires topographic index values from a DEM with a much finer grid cell resolution than the LIDAR data can provide, and the relationship is stronger in wetter conditions. In the forested environment, the DEM resolution required is considerably lower and adequately supported by the photogrammetric data, and the relationship is strong under all moisture conditions. These results provide some insights into the length scales of near‐surface hydrological processes in the urbanizing environment, and the resolution of terrain data required to model those processes. Copyright © 2006 John Wiley & Sons, Ltd. |
| doi_str_mv | 10.1002/hyp.5895 |
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In the forested environment, the DEM resolution required is considerably lower and adequately supported by the photogrammetric data, and the relationship is strong under all moisture conditions. These results provide some insights into the length scales of near‐surface hydrological processes in the urbanizing environment, and the resolution of terrain data required to model those processes. Copyright © 2006 John Wiley & Sons, Ltd.</description><identifier>ISSN: 0885-6087</identifier><identifier>EISSN: 1099-1085</identifier><identifier>DOI: 10.1002/hyp.5895</identifier><identifier>CODEN: HYPRE3</identifier><language>eng</language><publisher>Chichester, UK: John Wiley & Sons, Ltd</publisher><subject>Animal and plant ecology ; Animal, plant and microbial ecology ; Baltimore Ecosystem Study ; Biological and medical sciences ; digital elevation model ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Fundamental and applied biological sciences. 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E.</creatorcontrib><creatorcontrib>Band, L. E.</creatorcontrib><creatorcontrib>Kenworthy, S. T.</creatorcontrib><creatorcontrib>Tague, C. L.</creatorcontrib><title>Analysis of soil moisture patterns in forested and suburban catchments in Baltimore, Maryland, using high-resolution photogrammetric and LIDAR digital elevation datasets</title><title>Hydrological processes</title><addtitle>Hydrol. Process</addtitle><description>Field observations of near‐surface soil moisture, collected over several seasons in a watershed in suburban Maryland, are compared with values of the topographic soil moisture index generated using digital elevation models (DEMs) at a range of grid cell sizes from photogrammetric and light detection and ranging (LIDAR) data sources. A companion set of near‐surface soil moisture observations, DEMs and topographic index values are also presented for a nearby forested catchment. The degree to which topographic index values are an effective indicator of near‐surface soil moisture conditions varies in the two environments. The urbanizing environment requires topographic index values from a DEM with a much finer grid cell resolution than the LIDAR data can provide, and the relationship is stronger in wetter conditions. In the forested environment, the DEM resolution required is considerably lower and adequately supported by the photogrammetric data, and the relationship is strong under all moisture conditions. These results provide some insights into the length scales of near‐surface hydrological processes in the urbanizing environment, and the resolution of terrain data required to model those processes. 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Hydrogeology</subject><subject>LIDAR</subject><subject>resolution</subject><subject>soil moisture</subject><subject>Synecology</subject><subject>Terrestrial ecosystems</subject><subject>topographic index</subject><subject>urbanization</subject><issn>0885-6087</issn><issn>1099-1085</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNqF0stu1DAUgOEIgcRQkHgEb0AsmmI7cWwvhwLTSsNFqFBYWSeOMzE4cbCdlnkk3pLMRbBCXXnz6beOj7PsKcFnBGP6stuOZ0xIdi9bECxlTrBg97MFFoLlFRb8YfYoxu8Y4xILvMh-Lwdw22gj8i2K3jrUexvTFAwaISUThojsgFofTEymQTA0KE71FGoYkIaku94MaW9egUu2n-Epegdh62Z6iqZohw3q7KbL54J3U7J-QGPnk98E6HuTgtX76vry9fITauzGJnDIOHMDe9tAgmhSfJw9aMFF8-R4nmSf3765Or_I1x9Wl-fLdQ6MMJZLoTWBum4ko03ZcCaohqKuq7bEhvK6pW3RygKMIILVtaGEc0JK0LXGGhtcnGTPD90x-J_TPLXqbdTGzfMYP0VFZVnQqqB3QsIprqggd8OScyGLcoYvDlAHH2MwrRqD7ee3VASr3XbVvF212-5Mnx2bEDW4NsCgbfznOcO0kru784O7tc5s_9tTF98-HrtHP38C8-uvh_BDVbzgTF2_X6nrr6RYsasvShZ_ADGtxqI</recordid><startdate>20060215</startdate><enddate>20060215</enddate><creator>Tenenbaum, D. 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A companion set of near‐surface soil moisture observations, DEMs and topographic index values are also presented for a nearby forested catchment. The degree to which topographic index values are an effective indicator of near‐surface soil moisture conditions varies in the two environments. The urbanizing environment requires topographic index values from a DEM with a much finer grid cell resolution than the LIDAR data can provide, and the relationship is stronger in wetter conditions. In the forested environment, the DEM resolution required is considerably lower and adequately supported by the photogrammetric data, and the relationship is strong under all moisture conditions. These results provide some insights into the length scales of near‐surface hydrological processes in the urbanizing environment, and the resolution of terrain data required to model those processes. Copyright © 2006 John Wiley & Sons, Ltd.</abstract><cop>Chichester, UK</cop><pub>John Wiley & Sons, Ltd</pub><doi>10.1002/hyp.5895</doi><tpages>22</tpages></addata></record> |
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| subjects | Animal and plant ecology Animal, plant and microbial ecology Baltimore Ecosystem Study Biological and medical sciences digital elevation model Earth sciences Earth, ocean, space Exact sciences and technology Fundamental and applied biological sciences. Psychology Hydrology Hydrology. Hydrogeology LIDAR resolution soil moisture Synecology Terrestrial ecosystems topographic index urbanization |
| title | Analysis of soil moisture patterns in forested and suburban catchments in Baltimore, Maryland, using high-resolution photogrammetric and LIDAR digital elevation datasets |
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