Karen W. Holmes
Current Organizations / Institutes
The organizations/institutes from the scholar's latest article
Research Subjects
Karen W. Holmes has a total of 8 co-authors. Here are the top co-authors by number of shared publications:
Dar A. Roberts
Geography Department University of California Santa Barbara California USA
2 shared publicationsJoão Vianei Soares
Instituto de Pesquisas Espacias (INPE) Sao Jose dos Campos Brazil
2 shared publicationsOliver A. Chadwick
Geography Department University of California Santa Barbara California USA
2 shared publications- Phaedon C. Kyriakidis
Department of Civil Engineering and Geomatics, Cyprus University of Technology, Limassol 3036, Cyprus
2 shared publications B. Radford
School of Earth and Geographical Sciences, The University of Western Australia, Crawley, WA 6009, Australia
1 shared publicationEliomar P. Silva de Filho
Departamento de Geografía Universidade Federal de Rondônia (UNIR) Porto Velho Brazil
1 shared publication
Latest Publications
- 2 April 2008
- Published by Springer Nature in Landscape Ecology
- Vol. 23 (8)
N. Uphoff, A. S. Ball, E. Fernandes, H. Herren, O. Husson, M. Laing, C. Palm, J. Pretty, P. Sanchez, N. Sanginga, and J. Thies (eds.): Coupling Soil Process Research with Humanitarian and Environmental Values: Review of “Biological Approaches to Sustainable Soil Systems”
- 2 April 2008
- Published by Springer Nature in Landscape Ecology
- Vol. 23 (8)
N. Uphoff, A. S. Ball, E. Fernandes, H. Herren, O. Husson, M. Laing, C. Palm, J. Pretty, P. Sanchez, N. Sanginga, and J. Thies (eds.): Coupling Soil Process Research with Humanitarian and Environmental Values: Review of “Biological Approaches to Sustainable Soil Systems”
- 18 July 2006
- Published by American Geophysical Union (AGU) in Global Biogeochemical Cycles
- Vol. 20 (3)
Large‐area spatially explicit estimates of tropical soil carbon stocks and response to land‐cover change
Studies of tropical soil organic carbon (SOC) response to deforestation present conflicting results, confounding estimates of the regional effects of land‐cover change on carbon storage. We calculated the change in SOC stocks due to deforestation through 1996 for the state of Rondônia, Brazil, in the southwestern Amazon basin. Whereas the net change in SOC for the state as a whole was slightly negative (−0.5% or −5012 Gg), spatially explicit maps suggest dramatic local changes, ranging from −76% to +74%, with outliers as high as +330%. The direction and magnitude of change in SOC following forest clearing is related to original forest soil carbon and pH, which in turn provides a general measure for overall nutrient availability and possible toxicities. When native soil carbon is high, SOC decreases in response to land‐cover conversion from forest to pasture; conversely, low soil carbon and low soil fertility lead to gains in carbon under pasture. Mapping variability, rather than relying on large‐area averages, illustrates why results from individual field sites have been contradictory.
- 18 July 2006
- Published by American Geophysical Union (AGU) in Global Biogeochemical Cycles
- Vol. 20 (3)
Large‐area spatially explicit estimates of tropical soil carbon stocks and response to land‐cover change
Studies of tropical soil organic carbon (SOC) response to deforestation present conflicting results, confounding estimates of the regional effects of land‐cover change on carbon storage. We calculated the change in SOC stocks due to deforestation through 1996 for the state of Rondônia, Brazil, in the southwestern Amazon basin. Whereas the net change in SOC for the state as a whole was slightly negative (−0.5% or −5012 Gg), spatially explicit maps suggest dramatic local changes, ranging from −76% to +74%, with outliers as high as +330%. The direction and magnitude of change in SOC following forest clearing is related to original forest soil carbon and pH, which in turn provides a general measure for overall nutrient availability and possible toxicities. When native soil carbon is high, SOC decreases in response to land‐cover conversion from forest to pasture; conversely, low soil carbon and low soil fertility lead to gains in carbon under pasture. Mapping variability, rather than relying on large‐area averages, illustrates why results from individual field sites have been contradictory.
- 14 July 2006
- Published by Wiley in Aquatic Conservation: Marine and Freshwater Ecosystems
- Vol. 17 (4) , 385-407
Probabilistic large‐area mapping of seagrass species distributions
Aerial photograph classification was used to map perennial thick canopy seagrass presence/absence over a large area (85 km2) off the coast of Western Australia. Within those areas mapped as seagrass, a geostatistical nonparametric interpolation method was applied to map the probability of seagrass species presence from underwater tow video. Multiple species mixtures were mapped at fixed probability thresholds of 0.95, 0.75, 0.50, and 0.25. Taxa included Amphibolis spp., Posidonia coriacea, P. sinuosa, P. australis and ephemeral species (Halophila and Zostera tasmanica (newly named as Heterozostera polychlamys)). The most commonly occurring species were respectively Amphibolis spp., Posidonia coriacea, P. sinuosa, P. australis, and the ephemeral species. Amphibolis, P. coriacea, and the ephemeral species were mapped predominantly as mixed assemblages (71–89% mixed), whereas P. sinuosa and P. australis were typically mapped as single species. Different species growth habits led to distinctive differences in large area distributions. All species were highly variable over short distances (Posidonia sinuosa meadows were oriented with the longest axis running north–south, and a shorter axis running east–west perpendicular to the coastline (spatial dependence to 2.8 km and 0.8 km, respectively). The ephemeral species were less successfully mapped, largely owing to the potentially different growth patterns of the grouped species, and because their full extent could not be captured by the aerial photograph classification. The individual biology of each species results in unique landscape features where Posidonia sinuosa forms larger continuous and predominantly monospecific meadows, whereas the more common Amphibolis and P. coriacea form multi‐species patchy meadows. These mapped features suggest that the emergence of species patterns in seagrass landscapes is influenced by differences in clonal growth among seagrass species. Probabilistic species mapping provided information unavailable from discretely classified maps, and facilitates targeted sampling for improving map accuracy, and for more realistically evaluating species and mixed species distribution predictions. The kriging approach, although not well suited for all types of vegetation data, performed well for clonal seagrasses. Copyright © 2006 John Wiley & Sons, Ltd.
- 14 July 2006
- Published by Wiley in Aquatic Conservation: Marine and Freshwater Ecosystems
- Vol. 17 (4) , 385-407
Probabilistic large‐area mapping of seagrass species distributions
Aerial photograph classification was used to map perennial thick canopy seagrass presence/absence over a large area (85 km2) off the coast of Western Australia. Within those areas mapped as seagrass, a geostatistical nonparametric interpolation method was applied to map the probability of seagrass species presence from underwater tow video. Multiple species mixtures were mapped at fixed probability thresholds of 0.95, 0.75, 0.50, and 0.25. Taxa included Amphibolis spp., Posidonia coriacea, P. sinuosa, P. australis and ephemeral species (Halophila and Zostera tasmanica (newly named as Heterozostera polychlamys)). The most commonly occurring species were respectively Amphibolis spp., Posidonia coriacea, P. sinuosa, P. australis, and the ephemeral species. Amphibolis, P. coriacea, and the ephemeral species were mapped predominantly as mixed assemblages (71–89% mixed), whereas P. sinuosa and P. australis were typically mapped as single species. Different species growth habits led to distinctive differences in large area distributions. All species were highly variable over short distances (Posidonia sinuosa meadows were oriented with the longest axis running north–south, and a shorter axis running east–west perpendicular to the coastline (spatial dependence to 2.8 km and 0.8 km, respectively). The ephemeral species were less successfully mapped, largely owing to the potentially different growth patterns of the grouped species, and because their full extent could not be captured by the aerial photograph classification. The individual biology of each species results in unique landscape features where Posidonia sinuosa forms larger continuous and predominantly monospecific meadows, whereas the more common Amphibolis and P. coriacea form multi‐species patchy meadows. These mapped features suggest that the emergence of species patterns in seagrass landscapes is influenced by differences in clonal growth among seagrass species. Probabilistic species mapping provided information unavailable from discretely classified maps, and facilitates targeted sampling for improving map accuracy, and for more realistically evaluating species and mixed species distribution predictions. The kriging approach, although not well suited for all types of vegetation data, performed well for clonal seagrasses. Copyright © 2006 John Wiley & Sons, Ltd.
- 1 June 2005
- Published by Springer Nature in Biogeochemistry
- Vol. 74 (2) , 173-203
Multi-scale variability in tropical soil nutrients following land-cover change
- 1 June 2005
- Published by Springer Nature in Biogeochemistry
- Vol. 74 (2) , 173-203
Multi-scale variability in tropical soil nutrients following land-cover change