Research Papers

However, increasing anthropogenic intervention in the recent times appears to be contributing to terrain instability in addition to natural factors, as observed by increasing frequency and magnitude of landslides since 1970.

During August and September 2010, Uttarakhand Himalaya witnessed large-scale slope destabilization, particularly along the roads where widening work was in progress leading to huge damage. The cause of regional-scale landslides has been attributed to exceptionally high rainfall in the region during September. When the average rainfall for the month of August and September from 2000 to 2009 is compared with rainfall data of the same period of 2010, it was found that in September 2010, 336 per cent higher rainfall was received by the area. However, the question that arises is: was it unusual rainfall-induced calamity or a result of human intervention?

The study area was located in Halol Range,Panchmahal District, Gujarat, stretching between long. 22°25′41″N and 22°29′06″N, and lat. 73°31′23″E and 73°35′35″E. Preservation plots present in the study area were selected for the current study.

It explores the understanding of the local controls on the retreat of glaciers of the Baspa valley in Himachal Pradesh. The geomorphic records mapped are accumulation zone, exposed ablation zone, moraine-covered ablation zone, snout, deglaciated valley, lateral moraine, medial moraine, terminal moraine and hanging glacier.

Fluoride is essential for normal bone growth, but its higher concentration in drinking water poses great health problems and fluorosis is common in many parts of India.

The decision to act or not act, and further how to act in the face of unknowns or uncertainties is the subject matter of the precautionary principle (PP). It is against this historical backdrop of unknowns in environmental governance that the present study on the precautionary principle was conducted.

The present framework for environmental governance provides a number of areas where precaution can and must be applied. In addition to these areas, the present report is the outcome of a descriptive study that shows the extent to which key elements of the precautionary principle are embedded in the specific case of two environmental laws related to coasts. The study examines key areas of the clearance continuum (law-making, clearance and monitoring) through a single broad question: To what extent is the approach of precaution embedded in decision-making under the CRZ Notification 1991 and the Water Act, 1974?

Sridhar attempted to examine this question on a continuum that examines a) the text of the law, b) the conditions under which projects are cleared or rejected and c) issues related to the monitoring of these conditions. The Asia and Pacific Workshop Report of the Precautionary Principle Project declared that there are both explicit and implicit uses of the precautionary principle. It states that there are some instances where the PP’s application is explicit and unambiguous whereas in other decisions the PP is implicit. They also raise an important point that to actually determine whether a decision was indeed precautionary or not (where it is not explicit) requires an examination of the context and motivations for decisions and management interventions.

Groundwater is a natural replenishable resource. It is an important source for various purposes, including drinking, irrigation and industrial, due to insufficient surface water supply and frequent failure of monsoon. Identification of groundwater zones depends upon many factors such as distribution of rainfall, runoff, grain size of soil, topographic features, type of landform, drainage conditions, lithological characteristics, land use practices, depth to groundwater level and environmental constraints, which are not uniform in any area. 

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The paper informs that the conventional wisdom that ‘more forest is always better’ has dominated policy making in the management of forested watersheds. In the context of the supposed hydrological regulation service provided by forest ecosystems, however, hydrologists have debated this assumption for more than two decades.

This report by the Water and Sanitation Management Organisation (WASMO) is based on the analysis of Multi-District Assessment of Water Safety (M-DAWS) carried out in 8 districts of Gujarat (Vadodara,Valsad, Mehsana, Gandhinagar, Kachchh, Surat, Ahmedabad and Dangs) , where ensuring adequate and safe drinking water to the people has been looked upon as a huge challenge needing urgent action during years 2007 and 2008 .

The Multi-District Assessment of Water Safety (M-DAWS) programme was undertaken by Water and Sanitation Management Organisation (WASMO) with financial and technical support from UNICEF.

 Mountain areas and communities are susceptible to climate change. This work also yielded evidence of the coping strategies developed by the communities to deal with an unprecedented and only partially understood threat. This paper describes these strategies and attempts to assess the vulnerability of the communities in each valley.

The study on “Snow and Glacier Studies”  was taken up by the Space Applications Centre, Indian Space Research Organisation (ISRO) and executed in collaboration with fourteen research organizations and academic institutions of the country, at the behest of the Ministry of Environment and Forests.

 Himalayan mountains contain important natural resources of frozen fresh water in the form of snow and glaciers. These glaciers are unique as they are located in tropics, high altitude regions, predominantly valley type and many are covered with debris.

The great northern plains of India sustain on the perennial melt of snow and glaciers meeting the water requirements of agriculture, industries, domestic sector even in the months of summer when large tracts of the country go dry. Therefore, it is important to monitor and assess the state of snow and glaciers and to know the sustainability of glaciers in view of changing global scenarios of climate and water security of the nation. Any information pertaining to Himalayan glaciers is normally difficult to be obtained by conventional means due to its harsh weather and rugged terrains.