Delineating hydrological response units in a mountainous catchment and its evaluation on water mass balance and model performance

2014 ◽  
Author(s):  
Eleni Savvidou ◽  
Ourania Tzoraki ◽  
Dimitrios Skarlatos
Keyword(s):  
Mass Balance ◽  
Water Mass ◽  
Model Performance ◽  
Hydrological Response ◽  
Mountainous Catchment ◽  
Water Mass Balance

scholarly journals Industrial water mass balance as a tool for water management in industrial parks

2016 ◽  
Vol 13 ◽  
pp. 14-21 ◽  
Author(s):  
Thanh Tuan Pham ◽  
Thanh Dung Mai ◽  
Tien Duc Pham ◽  
Minh Trang Hoang ◽  
Manh Khai Nguyen ◽  
...  
Keyword(s):  
Water Management ◽  
Mass Balance ◽  
Water Mass ◽  
Industrial Water ◽  
Industrial Parks ◽  
Water Mass Balance

Urban Water Mass Balance Analysis

2011 ◽  
Vol 15 (5) ◽  
pp. 693-706 ◽  
Author(s):  
Steven Kenway ◽  
Alan Gregory ◽  
Joseph McMahon
Keyword(s):  
Mass Balance ◽  
Water Mass ◽  
Urban Water ◽  
Balance Analysis ◽  
Water Mass Balance ◽  
Mass Balance Analysis

scholarly journals Estimate of Greenland and Antarctic ice-sheet total discharge from multiple GRACE solutions

2019 ◽  
Author(s):  
Ida Russo ◽  
Guillaume Ramillien ◽  
Frédéric Frappart ◽  
Frédérique Rémy
Keyword(s):  
Mass Balance ◽  
Climate Model ◽  
Water Mass ◽  
Drainage Basin ◽  
Ice Sheets ◽  
Ice Sheet ◽  
Gravimetric Data ◽  
Water Mass Balance ◽  
Processing Techniques ◽  
Total Discharge

Abstract. In this work a method for the estimation of 2003–2010 monthly-mean total discharge from Greenland and Antarctica is presented. We show that measurements of time-variable gravity from GRACE when combined with estimates of precipitation and sublimation can realistically reconstruct the total discharge from the ice-sheets into the ocean. In particular, the total discharge has been calculated as a 8-member ensemble-mean obtained by combining multiple GRACE solutions with water fluxes from both an high resolution regional atmospheric climate model (RACMO2) and a global reanalysis (ERA-Interim). The gravimetric measurements of mass variations and the precipitation and sublimation atmospheric fields have been combined in the ice-sheets water mass balance equation, according to the main drainage basin systems. The use of the combined land-atmosphere water mass balance has also been tested, which however led to a large underestimation of total discharge. A comparison among the different GRACE solutions is also performed, highlighting similarities and differences and analyzing the possible causes. GRACE datasets show similar ice-sheet mass trends on Antarctica and over the majority of the Greenland basins, while significant differences (up to a factor of 1.9) have been found in mass-loss areas characterized by strongly negative water height trends. This is likely primarily caused by the different pre-processing techniques applied to the raw gravimetric data.

scholarly journals Supplemental Material: Conservative transport of dissolved sulfate across the Rio Madre de Dios floodplain in Peru

2021 ◽  
Author(s):  
Emily Burt ◽  
et al.
Keyword(s):  
Mass Balance ◽  
Oxygen Isotope ◽  
Water Mass ◽  
Mixing Model ◽  
Geochemical Data ◽  
Madre De Dios ◽  
Water Mass Balance

Details on the chloride-based mixing model and oxygen isotope calculations, Table S1 (geochemical data), and Table S2 (sulfate and water mass balance calculations).<br>

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