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GLACIER ICE MASS CHANGES IN CENTRAL HIMALAYAS DURING 2000-2014 USING TanDEM- X DATA
Glacier elevation change TanDEM-X SRTM geodetic mass balance Central Indian Himalaya
2019/2/27
The Himalayas have been widely accepted as one of the most sensitive indicators of climate change. However, the rugged terrains of the Indian Himalayas render it impossible to carry out ground based s...
STUDY OF AEROSOL OPTICAL PROPERTIES OVER TWO SITES IN THE FOOTHILLS OF THE CENTRAL HIMALAYAS
AOD angstrom exponent urban industrial biomass burning Central Himalayas
2018/5/15
Atmospheric aerosol possesses impacts on climate system and ecological environments, human health and agricultural productivity. The environment over Himalayas and Tibetan Plateau region are continuou...
Attenuation of P, S and Coda Waves in the NW-Himalayas, India
Attenuation Quality Factor Frequency Dependence NW Himalayas
2013/3/7
The frequency-dependent characteristics of P- and S-wave attenuation in the upper crust of NW Himalayas have been estimated using local earthquakes for a frequency range of 1.5 to 18 Hz. A total of 43...
Chemical composition and aerosol size distribution of the middle mountain range in the Nepal Himalayas during the 2009 pre-monsoon season
Chemical composition aerosol size the middle mountain range the Nepal Himalayas the 2009 pre-monsoon season
2010/12/28
Aerosol particle number size distribution and chemical composition were measured at two low altitude sites, one urban and one relatively pristine valley, in Central Nepal during the 2009 pre-monsoon s...
Aerosol mass and black carbon concentrations, a two year record at NCO-P (5079 m, Southern Himalayas)
Aerosol mass black carbon NCO-P
2010/9/21
Aerosol mass and the absorbing fraction are important variables, needed to constrain the role of atmospheric particles in the Earth radiation budget, both directly and indirectly through CCN activatio...
Joint spatial variability of aerosol, clouds and rainfall in the Himalayas from satellite data
aerosol clouds rainfall the Himalayas satellite data
2010/9/21
Satellite-based precipitation, Aerosol Optical Depth (AOD), Cloud Optical Depth (COD), and Aerosol Index (AI) data were used to characterize the linkages among landform and the intra-annual variabilit...
Tropospheric ozone variations at the Nepal Climate Observatory-Pyramid (Himalayas, 5079 m a.s.l.) and influence of deep stratospheric intrusion events
Tropospheric ozone the Nepal Climate Observatory-Pyramid deep stratospheric intrusion events
2010/8/16
The paper presents the first 2 years of continuous surface ozone (O3) observations and systematic assessment of the influence of stratospheric intrusions (SI) at the Nepal Climate Observatory at Pyram...
Utilization of Satellite Snow-Cover Observations for Seasonal Streamflow Estimates in the Western Himalayas
Satellite Snow-Cover Observations Seasonal Streamflow Estimates Western Himalayas
2009/10/28
The results presented in this study indicate the possibility of seasonal runoff
prediction when satellite-derived basin snow-cover data are related to point
source river discharge data for a number ...
Evaluating a Model of Snow Cover Area versus Runoff against a Concurrent Flow Correlation Model in the Western Himalayas
Snow Cover Area versus Runoff Concurrent Flow Correlation Model
2009/10/28
This study evaluates the estimates of seasonal snowmelt runoff in the Sutlej,
Indus, Kabul and Chenab rivers derived from the model of snow cover area
vs. runoff against those obtained from cross co...
A Test of Snowmelt-Runoff Model for a Major River Basin in Western Himalayas
Snowmelt-Runoff Model Major River Basin Western Himalayas
2009/10/27
In the Snowmelt-Runoff Model (SRM), the estimate of discharge volume is
based on temperature condition in the form of degree days which are used to
melt the snowpack in the area of the basin covered...
Linear or Nonlinear Covariance of Seasonal Snowmelt and Snow Cover in Western Himalayas
Nonlinear Covariance Seasonal Snowmelt Snow Cover Western Himalayas
2009/10/26
Log-linear, exponential and fractional relations for estimating seasonal snowmelt
from early-spring snow accumulation in the Indus and Kabul river basins
in the western Himalayas are developed with ...
Topographical Influence on Precipitation Distribution in Different Ranges of Western Himalayas
Topographical Influence Precipitation Distribution Western Himalayas
2009/10/26
Seasonal and annual distribution of rainfall and snowfall with elevation has been
studied for outer, middle and greater Himalayan ranges of Chenab basin in the
western Himalayas. Rainfall and snowfa...
A Simple Monthly Runoff Model for Snow Dominated Catchments in Western Himalayas
Monthly Runoff Model Snow Dominated Catchments Western Himalayas
2009/10/23
The rivers originating from middle and greater Himalayas have a significant part
of their catchments under permanent snow cover and glaciers. Modeling runoff
becomes difficult with almost no data fr...
A Study of Sedimentation in Chenab Basin in Western Himalayas
Sedimentation Chenab Basin Western Himalayas
2009/10/23
The young Himalayas have a serious problem of soil erosion arid consequent
sedimentation in river reaches downstream. The study revealed the high rates of
sedimentation in Chenab basin and its effec...
Suspended Sediment Transport from the Dokriani Glacier in the Garhwal Himalayas
Suspended Sediment Transport Dokriani Glacier Garhwal Himalayas
2009/10/22
Estimation of sediment load from glacierized basins is very important for planning,
designing, installation and operation of hydro-power projects, including
management of reservoirs. In the present ...