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Libros sobre el tema "Geomorphic processes"

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Autor: Grafiati
Publicado: 4 de junio de 2021
Última modificación: 20 de febrero de 2023

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1

Dorava, Joseph M., David R. Montgomery, Betty B. Palcsak y Faith A. Fitzpatrick, eds. Geomorphic Processes and Riverine Habitat. Washington, D. C.: American Geophysical Union, 2001. http://dx.doi.org/10.1029/ws004.

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2

Damm, Bodo, Heinrich Thiemeyer y Birgit Terhorst. Hillslope processes in geomorphic systems on varying temporal and spatial scales. Stuttgart: Gebrüder Borntraeger, 2012.

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3

Simon, Andrew. Geomorphic and vegetative recovery processes along modified stream channels of west Tennessee. Nashville, Tenn: U.S. Geological Survey, 1992.

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4

Gustavson, Thomas C. Geomorphic processes and rates of retreat affecting the Caprock Escarpment, Texas Panhandle. Austin, Tex: Bureau of Economic Geology, University of Texas at Austin, 1989.

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5

Simon, Andrew. Geomorphic and vegetative recovery processes along modified stream channels of west Tennessee. Nashville, Tenn: U.S. Geological Survey, 1992.

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6

Simon, Andrew. Geomorphic and vegetative recovery processes along modified stream channels of west Tennessee. Nashville, Tenn: U.S. Geological Survey, 1992.

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7

Simon, Andrew. Geomorphic and vegetative recovery processes along modified stream channels of west Tennessee. Washington, D.C: U.S. G.P.O., 1994.

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8

Gustavson, Thomas C. Geomorphic processes and rates of retreat affecting the Caprock Escarpment, Texas Panhandle. Austin, TX: University of Texas at Austin, 1989.

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9

Molinelli, Joseph Antonio. Geomorphic processes along the Autopista Las Americas in North Central Puerto Rico: Implications for highway construction, design and maintenance. Ann Arbor, Mich: University Microfilms International, 1990.

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10

Branson, Farrel Allen. Contrasts of vegetation, soils, microclimates, and geomorphic processes between north- and south-facing slopes on Green Mountain near Denver, Colorado. Denver, Colo: Dept. of the Interior, U.S. Geological Survey, 1990.

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11

Regional Conference on Mediterranean Countries (1986 Barcelona, Spain). Geomorphic processes in environments with strong seasonal contrasts: Selected papers of the Regional Conference on Mediterranean Countries, IGU Commission on Measurement, Theory and Application in Geomorphology, Barcelona-Valencia-Murcia-Granada, September 5-14, 1986. Cremlingen-Destedt, W. Germany: Catena, 1988.

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12

International, Symposium on Coastal Engineering and Science of Coastal Sediment Processes (4th 1999 Hauppauge N. Y. ). Coastal sediments '99: Proceedings of the 4th International Symposium on Coastal Engineering and Science of Coastal Sediment Processes : confrence theme : scales of coastal sediment motion and geomorphic change, Hauppauge, Long Island, New York, June 21-23, 1999. Reston, VA: American Society of Civil Engineers, 1999.

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13

Palcsak, Betty B., David R. Montgomery, Faith A. Fitzpatrick y Joseph M. Dorava. Geomorphic Processes and Riverine Habitat. Wiley & Sons, Limited, John, 2013.

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14

(Editor), A. M. Harvey y M. Sala (Editor), eds. Geomorphic Processes in Environments with Strong Seasonal Contrasts, Vol. II: Geomorphic Systems (Catena Supplement 13). Catena-Verlag, 1988.

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15

Evaluation of Bridge Scour Research: Geomorphic Processes and Predictions. Washington, D.C.: Transportation Research Board, 2011. http://dx.doi.org/10.17226/22884.

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16

(Editor), Joseph M. Dorava, David R. Montgomery (Editor), Betty B. Palcsak (Editor) y Faith A. Fitzpatrick (Editor), eds. Geomorphic Processes and Riverine Habitat (Water Science and Application, 4). American Geophysical Union, 2001.

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17

Dietrich, Barsch, Mäusbacher Roland y Deutscher Arbeitskreis für Geomorphologie, eds. Some contributions to the study of landforms and geomorphic processes. Berlin: Gebrüder Borntraeger, 1993.

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18

(Editor), A. C. Imeson y M. Sala (Editor), eds. Geomorphic Processes in Environments with Strong Seasonal Contrasts, Vol. I: Hillslope Processes (Catena Supplement 12). Catena-Verlag, 1988.

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19

Geomorphic, sedimentologic and chronologic analysis of the Opal Dune Field, Lincoln County, Wyoming. [Denver, CO]: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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20

1949-, Nolan K. M., Kelsey H. M y Marron D. C, eds. Geomorphic processes and aquatic habitat in the Redwood Creek Basin, northwestern California. Washington: U.S. G.P.O., 1995.

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21

Geomorphic processes and aquatic habitat in the Redwood Creek Basin, northwestern California. Washington, DC: U.S. Government Printing Office, 1992.

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22

Nolan, K. M., H. M. Kelsey y D. C. Marron. 'Geomorphic Processes and Aquatic Habitat in the Redwood Creek Basin, Northwestern California (Geological Survey Professional Paper 1454)'. U.S. Geological Survey, 1995.

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23

Hupp, C. R. y Andrew Simon. Geomorphic and Vegetative Recovery Processes Along Modified Stream Channels of West Tennessee (U.S. Geological Survey Open File Report: 91-0502). U S Geological Survey, 1997.

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24

Geological Survey (U.S.), ed. Changes in channel-stored sediment, Redwood Creek, northwestern California 1947 to 1980: Geomorphic processes and aquatic habitat in the Redwood Creek basin, northwestern California. [Sacramento, CA]: U.S. Geological Survey, 1992.

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25

Hazarika, Manjil. The Archaeological Record. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199474660.003.0005.

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This chapter elaborates the data and results of the explorations conducted in the Garbhanga Reserve Forest. The area has been intensively surveyed for the location of potential archaeological sites and the collection of ethnographic data in order to draw direct historical analogies. An ‘area-approach’ study has been conducted in order to formulate a general model for archaeological site structure, locations, geomorphic situations, and site formation processes that can be used for archaeological study in the hilly landscape of Northeast India. Present-day agricultural implements have been analysed and compared with Neolithic implements in order to reconstruct ancient farming culture by way of undertaking systematic study of modern peasant ways of life in the study area. The ideological significance of stone artefacts as ‘thunderstone’ in Northeast India and among the Karbis has also been discussed.
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26

Xue, Yongkang, Yaoming Ma y Qian Li. Land–Climate Interaction Over the Tibetan Plateau. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.592.

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The Tibetan Plateau (TP) is the largest and highest plateau on Earth. Due to its elevation, it receives much more downward shortwave radiation than other areas, which results in very strong diurnal and seasonal changes of the surface energy components and other meteorological variables, such as surface temperature and the convective atmospheric boundary layer. With such unique land process conditions on a distinct geomorphic unit, the TP has been identified as having the strongest land/atmosphere interactions in the mid-latitudes.Three major TP land/atmosphere interaction issues are presented in this article: (1) Scientists have long been aware of the role of the TP in atmospheric circulation. The view that the TP’s thermal and dynamic forcing drives the Asian monsoon has been prevalent in the literature for decades. In addition to the TP’s topographic effect, diagnostic and modeling studies have shown that the TP provides a huge, elevated heat source to the middle troposphere, and that the sensible heat pump plays a major role in the regional climate and in the formation of the Asian monsoon. Recent modeling studies, however, suggest that the south and west slopes of the Himalayas produce a strong monsoon by insulating warm and moist tropical air from the cold and dry extratropics, so the TP heat source cannot be considered as a factor for driving the Indian monsoon. The climate models’ shortcomings have been speculated to cause the discrepancies/controversies in the modeling results in this aspect. (2) The TP snow cover and Asian monsoon relationship is considered as another hot topic in TP land/atmosphere interaction studies and was proposed as early as 1884. Using ground measurements and remote sensing data available since the 1970s, a number of studies have confirmed the empirical relationship between TP snow cover and the Asian monsoon, albeit sometimes with different signs. Sensitivity studies using numerical modeling have also demonstrated the effects of snow on the monsoon but were normally tested with specified extreme snow cover conditions. There are also controversies regarding the possible mechanisms through which snow affects the monsoon. Currently, snow is no longer a factor in the statistic prediction model for the Indian monsoon prediction in the Indian Meteorological Department. These controversial issues indicate the necessity of having measurements that are more comprehensive over the TP to better understand the nature of the TP land/atmosphere interactions and evaluate the model-produced results. (3) The TP is one of the major areas in China greatly affected by land degradation due to both natural processes and anthropogenic activities. Preliminary modeling studies have been conducted to assess its possible impact on climate and regional hydrology. Assessments using global and regional models with more realistic TP land degradation data are imperative.Due to high elevation and harsh climate conditions, measurements over the TP used to be sparse. Fortunately, since the 1990s, state-of-the-art observational long-term station networks in the TP and neighboring regions have been established. Four large field experiments since 1996, among many observational activities, are presented in this article. These experiments should greatly help further research on TP land/atmosphere interactions.
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