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Hydraulics of Time-Variable Water Surface Slope in Rivers Observed by Satellite Altimetry
The ICESat-2 and SWOT satellite earth observation missions have provided highly accurate water surface slope (WSS) observations in global rivers for the first time. While water surface slope is expected to remain constant in time for approximately uniform flow conditions, we observe time varying wat...
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Published in: | Remote sensing (Basel, Switzerland) Switzerland), 2024-11, Vol.16 (21), p.4010 |
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description | The ICESat-2 and SWOT satellite earth observation missions have provided highly accurate water surface slope (WSS) observations in global rivers for the first time. While water surface slope is expected to remain constant in time for approximately uniform flow conditions, we observe time varying water surface slope in many river reaches around the globe in the ICESat-2 record. Here, we investigate the causes of time variability of WSSs using simplified river hydraulic models based on the theory of steady, gradually varied flow. We identify bed slope or cross section shape changes, river confluences, flood waves, and backwater effects from lakes, reservoirs, or the ocean as the main non-uniform hydraulic situations in natural rivers that cause time changes of WSSs. We illustrate these phenomena at selected river sites around the world, using ICESat-2 data and river discharge estimates. The analysis shows that WSS observations from space can provide new insights into river hydraulics and can enable the estimation of river discharge from combined observations of water surface elevation and WSSs at sites with complex hydraulic characteristics. |
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While water surface slope is expected to remain constant in time for approximately uniform flow conditions, we observe time varying water surface slope in many river reaches around the globe in the ICESat-2 record. Here, we investigate the causes of time variability of WSSs using simplified river hydraulic models based on the theory of steady, gradually varied flow. We identify bed slope or cross section shape changes, river confluences, flood waves, and backwater effects from lakes, reservoirs, or the ocean as the main non-uniform hydraulic situations in natural rivers that cause time changes of WSSs. We illustrate these phenomena at selected river sites around the world, using ICESat-2 data and river discharge estimates. The analysis shows that WSS observations from space can provide new insights into river hydraulics and can enable the estimation of river discharge from combined observations of water surface elevation and WSSs at sites with complex hydraulic characteristics.</description><identifier>ISSN: 2072-4292</identifier><identifier>EISSN: 2072-4292</identifier><identifier>DOI: 10.3390/rs16214010</identifier><language>eng</language><publisher>Basel: MDPI AG</publisher><subject>Altimeter ; Backwater effect ; Data processing ; Earth observations (from space) ; Flood waves ; Flow velocity ; Fluid flow ; Friction ; Gradually-varied flow ; Hydraulic models ; Hydraulics ; ICESat-2 ; Measurement ; Methods ; River discharge ; River flow ; river hydraulics ; Rivers ; Satellite altimetry ; Satellite communications ; Satellite observation ; Shape effects ; Slopes (Physical geography) ; Uniform flow ; Varied flow ; Water ; Water discharge ; water surface slope</subject><ispartof>Remote sensing (Basel, Switzerland), 2024-11, Vol.16 (21), p.4010</ispartof><rights>COPYRIGHT 2024 MDPI AG</rights><rights>2024 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/). 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While water surface slope is expected to remain constant in time for approximately uniform flow conditions, we observe time varying water surface slope in many river reaches around the globe in the ICESat-2 record. Here, we investigate the causes of time variability of WSSs using simplified river hydraulic models based on the theory of steady, gradually varied flow. We identify bed slope or cross section shape changes, river confluences, flood waves, and backwater effects from lakes, reservoirs, or the ocean as the main non-uniform hydraulic situations in natural rivers that cause time changes of WSSs. We illustrate these phenomena at selected river sites around the world, using ICESat-2 data and river discharge estimates. The analysis shows that WSS observations from space can provide new insights into river hydraulics and can enable the estimation of river discharge from combined observations of water surface elevation and WSSs at sites with complex hydraulic characteristics.</description><subject>Altimeter</subject><subject>Backwater effect</subject><subject>Data processing</subject><subject>Earth observations (from space)</subject><subject>Flood waves</subject><subject>Flow velocity</subject><subject>Fluid flow</subject><subject>Friction</subject><subject>Gradually-varied flow</subject><subject>Hydraulic models</subject><subject>Hydraulics</subject><subject>ICESat-2</subject><subject>Measurement</subject><subject>Methods</subject><subject>River discharge</subject><subject>River flow</subject><subject>river hydraulics</subject><subject>Rivers</subject><subject>Satellite altimetry</subject><subject>Satellite communications</subject><subject>Satellite observation</subject><subject>Shape effects</subject><subject>Slopes (Physical geography)</subject><subject>Uniform flow</subject><subject>Varied flow</subject><subject>Water</subject><subject>Water discharge</subject><subject>water surface 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Karina</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Hydraulics of Time-Variable Water Surface Slope in Rivers Observed by Satellite Altimetry</atitle><jtitle>Remote sensing (Basel, Switzerland)</jtitle><date>2024-11-01</date><risdate>2024</risdate><volume>16</volume><issue>21</issue><spage>4010</spage><pages>4010-</pages><issn>2072-4292</issn><eissn>2072-4292</eissn><abstract>The ICESat-2 and SWOT satellite earth observation missions have provided highly accurate water surface slope (WSS) observations in global rivers for the first time. While water surface slope is expected to remain constant in time for approximately uniform flow conditions, we observe time varying water surface slope in many river reaches around the globe in the ICESat-2 record. Here, we investigate the causes of time variability of WSSs using simplified river hydraulic models based on the theory of steady, gradually varied flow. We identify bed slope or cross section shape changes, river confluences, flood waves, and backwater effects from lakes, reservoirs, or the ocean as the main non-uniform hydraulic situations in natural rivers that cause time changes of WSSs. We illustrate these phenomena at selected river sites around the world, using ICESat-2 data and river discharge estimates. 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subjects | Altimeter Backwater effect Data processing Earth observations (from space) Flood waves Flow velocity Fluid flow Friction Gradually-varied flow Hydraulic models Hydraulics ICESat-2 Measurement Methods River discharge River flow river hydraulics Rivers Satellite altimetry Satellite communications Satellite observation Shape effects Slopes (Physical geography) Uniform flow Varied flow Water Water discharge water surface slope |
title | Hydraulics of Time-Variable Water Surface Slope in Rivers Observed by Satellite Altimetry |
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