Modelling spatial and temporal variability of hydrologic impacts of climate change in the Fraser River basin, British Columbia, Canada

2012 ◽  
Vol 26 (12) ◽  
pp. 1840-1860 ◽  
Author(s):  
Rajesh R. Shrestha ◽  
Markus A. Schnorbus ◽  
Arelia T. Werner ◽  
Anne J. Berland
Keyword(s):  
Climate Change ◽  
British Columbia ◽  
River Basin ◽  
Temporal Variability ◽  
Spatial And Temporal Variability ◽  
Fraser River ◽  
Hydrologic Impacts ◽  
Impacts Of Climate Change

Assessment of hydrologic impacts of climate change in Tunga-Bhadra river basin, India with HEC-HMS and SDSM

2012 ◽  
Vol 27 (11) ◽  
pp. 1572-1589 ◽  
Author(s):  
R. Meenu ◽  
S. Rehana ◽  
P. P. Mujumdar
Keyword(s):  
Climate Change ◽  
River Basin ◽  
Hydrologic Impacts ◽  
Impacts Of Climate Change

Future Climate Change Impacts on Snow and Water Resources of the Fraser River Basin, British Columbia

2017 ◽  
Vol 18 (2) ◽  
pp. 473-496 ◽  
Author(s):  
Siraj ul Islam ◽  
Stephen J. Déry ◽  
Arelia T. Werner
Keyword(s):  
Climate Change ◽  
British Columbia ◽  
Snow Cover ◽  
River Basin ◽  
Snow Water Equivalent ◽  
Climate Change Impacts ◽  
Snow Accumulation ◽  
Low Flow ◽  
Future Climate Change ◽  
Fraser River

Abstract Changes in air temperature and precipitation can modify snowmelt-driven runoff in snowmelt-dominated regimes. This study focuses on climate change impacts on the snow hydrology of the Fraser River basin (FRB) of British Columbia (BC), Canada, using the Variable Infiltration Capacity model (VIC). Statistically downscaled forcing datasets based on 12 models from phase 5 of the Coupled Model Intercomparison Project (CMIP5) are used to drive VIC for two 30-yr time periods, a historical baseline (1980–2009) and future projections (2040–69: 2050s), under representative concentration pathways (RCPs) 4.5 and 8.5. The ensemble-based VIC simulations reveal widespread and regionally coherent spatial changes in snowfall, snow water equivalent (SWE), and snow cover over the FRB by the 2050s. While the mean precipitation is projected to increase slightly, the fraction of precipitation falling as snow is projected to decrease by nearly 50% in the 2050s compared to the baseline. Snow accumulation and snow-covered area are projected to decline substantially across the FRB, particularly in the Rocky Mountains. Onset of springtime snowmelt in the 2050s is projected to be nearly 25 days earlier than historically, yielding more runoff in the winter and spring for the Fraser River at Hope, BC, and earlier recession to low-flow volumes in summer. The ratio of snowmelt contribution to runoff decreases by nearly 20% in the Stuart and Nautley subbasins of the FRB in the 2050s. The decrease in SWE and loss of snow cover is greater from low to midelevations than in high elevations, where temperatures remain sufficiently cold for precipitation to fall as snow.

Hydrologic impacts of climate change on the Nile River Basin: implications of the 2007 IPCC scenarios

2009 ◽  
Vol 100 (3-4) ◽  
pp. 433-461 ◽  
Author(s):  
Tazebe Beyene ◽  
Dennis P. Lettenmaier ◽  
Pavel Kabat
Keyword(s):  
Climate Change ◽  
River Basin ◽  
Nile River ◽  
Hydrologic Impacts ◽  
Nile River Basin ◽  
Impacts Of Climate Change

scholarly journals Impacts of climate change and LULC change on runoff in the Jinsha River Basin

2020 ◽  
Vol 30 (1) ◽  
pp. 85-102 ◽  
Author(s):  
Qihui Chen ◽  
Hua Chen ◽  
Jun Zhang ◽  
Yukun Hou ◽  
Mingxi Shen ◽  
...  
Keyword(s):  
Climate Change ◽  
River Basin ◽  
Jinsha River ◽  
Lulc Change ◽  
Impacts Of Climate Change

scholarly journals Integrating Strategic Environmental Assessment to Climate Change Adaption in the Chao Phraya River Basin: Case Study Flood Management Plans in Ayutthaya

2021 ◽  
Vol 6 (2) ◽  
pp. p55
Author(s):  
Wilawan Boonsri Prathaithep ◽  
Vilas Nitivattananon
Keyword(s):  
Climate Change ◽  
River Basin ◽  
Environmental Assessment ◽  
Flood Risk ◽  
Assessment Tool ◽  
Flood Management ◽  
Integrated System ◽  
Strategic Environmental Assessment ◽  
Human Environment ◽  
Impacts Of Climate Change

Traditionally, flood management has concentrated on providing protection against floods using technical measures, but there is currently an international shift towards a more integrated system of flood risk management, whereby flood risk is defined as the probability of flooding multiplied by the potential consequences. Climate change is a great challenge to sustainable development and the Millennium Development Goals (MDGs) in Thailand. The main purpose of this paper is to highlight the challenges associated with the current situation and projected impacts of climate change on the disasters and the human environment in Thailand, to review and explore the potential of Strategic Environmental Assessment (SEA), and to propose SEA in making informed decisions relevant to the implementation of the new adaptation framework in a flood management plan. Thus, current measures on how Thailand is responding to the recent impacts of climate change in river basin planning are presented. It is imperative that an appropriate environmental assessment tool, such as SEA be employed in making rational decisions regarding adaptation frameworks. SEA offers a structured and proactive environmental tool for integrating of climate change adaption into formulating Policies, Plans, and Programs (PPPs) among relevant sectors.

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