Titlebook: Land Cover Change and Its Eco-environmental Responses in Nepal; Ainong Li,Wei Deng,Wei Zhao Book 2017 Springer Nature Singapore Pte Ltd. 2

Locale

Land Cover Mapping and Its Spatial Pattern Analysis in Nepal land, followed by croplands covering about 25%. The areal proportion of paddy fields to dry farmlands was approximately two to three. Topographical and meteorological factors presented as the determining effects on the spatial patterns of land cover in Nepal. With elevation uplift from south to nor

熄滅

Arteriography

Land Use Change and Its Driving Forces in the Koshi Hills, Eastern Nepald uses, such as arable land, forest, shrubland, grassland, and others (water bodies, snow land, bare land, rock and ice, settlement built-ups, and roads), have been determined, based on 1996 toposheets. In the Koshi Hills, significant changes have occurred particularly in forest land, with it increa

嚙齒動(dòng)物

Historical Land Covers Change in the Chure-Tarai Landscape in the Last Six Decades: Drivers and Envi Tarai, Bhawar, and Duns. Following from the eradication of malaria in the 1950s and 1960s, planned resettlement programs and the implementation of development projects attracted people from food-deficit conditions in the hills to the lowlands, causing a large-scale change in the land cover as well

獨(dú)行者

空氣傳播

Blemish

Assessments of Climate Change Indicators, Climate-Induced Disasters, and Community Adaptation Strateectively; precipitation is decreasing by 11.17?mm per annum with the erratic pattern. Melting of snow, occurrence of landslide and conversion of snow mountain to barren land and then vegetation are some distinctly noticed scenario associated with climate change. More than 25% people residing in the

使服水土

Geo-information-Based Soil Erosion Modeling for Sustainable Agriculture Development in Khadokhola Wawere found highly correlated with the slope of land system units. 64.41% of the total potential soil loss was mainly contributed only by land system unit 8 with the spatial coverage of 17% of the watershed area. This unit was characterized by steeply to very steeply sloping hilly and mountainous ter

煞費(fèi)苦心

137Cs Tracing Dynamics of Soil Erosion, Organic Carbon, and Total Nitrogen in Terraced Fields and Fo. Along the entire terraced toposequence, .Cs data showed that abrupt changes in soil erosion rates could occur between the lower part of the upper terrace and the upper part of the immediate terrace within a small distance. This result indicated that tillage erosion is also a dominant erosion type

猛然一拉