Ice and Other Debris - Revision history

Mpollei@gfnet.com at 04:51, 21 July 2023

2023-07-21T04:51:11Z

← Older revision		Revision as of 04:51, 21 July 2023
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	==Best Practices Resources==		==Best Practices Resources==
	{{Document Icon}} [[Ice Engineering (EM 1110-2-1612)\|Ice Engineering (EM 1110-2-1612), USACE~~, 2002~~]]		{{Document Icon}} [[Ice Engineering (EM 1110-2-1612)\|Ice Engineering (EM 1110-2-1612), USACE]]
	{{Document Icon}} [[Ice Pressure on Engineering Structures (CRREL III-B1b)\|Ice Pressure on Engineering Structures (CRREL III-B1b), USACE~~, 1970~~]]		{{Document Icon}} [[Ice Pressure on Engineering Structures (CRREL III-B1b)\|Ice Pressure on Engineering Structures (CRREL III-B1b), USACE]]

	<!-- For information on notation for in text citations visit https://www.mediawiki.org/wiki/Help:Cite Or simply enclose the citation as shown <ref> citation </ref> in the location of the in text mention. Citations will automatically populate below-->		<!-- For information on notation for in text citations visit https://www.mediawiki.org/wiki/Help:Cite Or simply enclose the citation as shown <ref> citation </ref> in the location of the in text mention. Citations will automatically populate below-->

Rmanwaring at 20:27, 19 December 2022

2022-12-19T20:27:03Z

← Older revision		Revision as of 20:27, 19 December 2022
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	<!-- Delete any sections that are not necessary to your topic. Add pictures/sections as needed -->		<!-- Delete any sections that are not necessary to your topic. Add pictures/sections as needed -->
	“Each year, ice grows on and disappears from the nation’s rivers and lakes in tune with cycles of nature. Unless the ice causes problems, such as flooding or blocking the arteries of commerce, few people pay more than cursory attention. Because of this, the very great variety of ways in which ice initially forms, grows, and accumulates, and finally disappears, are relatively unknown. Ice processes on lakes are different from those on rivers, and for both lakes and rivers, the size of the water body affects which processes take place. Ice owes its existence to the thermal process of heat transfer, but its evolution is greatly influenced by physical and mechanical processes”.<ref name="EM 1110-2-1612">[[Ice Engineering (EM 1110-2-1612) \| EM 1110-2-1612 ~~Ice Engineering~~, USACE, 2002]]</ref>		“Each year, ice grows on and disappears from the nation’s rivers and lakes in tune with cycles of nature. Unless the ice causes problems, such as flooding or blocking the arteries of commerce, few people pay more than cursory attention. Because of this, the very great variety of ways in which ice initially forms, grows, and accumulates, and finally disappears, are relatively unknown. Ice processes on lakes are different from those on rivers, and for both lakes and rivers, the size of the water body affects which processes take place. Ice owes its existence to the thermal process of heat transfer, but its evolution is greatly influenced by physical and mechanical processes”.<ref name="EM 1110-2-1612">[[Ice Engineering (EM 1110-2-1612) \| Ice Engineering (EM 1110-2-1612), USACE, 2002]]</ref>

	The formation, movement, and accumulation of ice in rivers and [[reservoirs]] at, or around, various hydraulic structures complicates the methods used to predict flooding, sediment transport, and scour, as well as complicates the [[operation]] and maintenance of different components of hydraulic structures such as gates, culverts, and bridges.		The formation, movement, and accumulation of ice in rivers and [[reservoirs]] at, or around, various hydraulic structures complicates the methods used to predict flooding, sediment transport, and scour, as well as complicates the [[operation]] and maintenance of different components of hydraulic structures such as gates, culverts, and bridges.
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	{{Website Icon}} [https://damfailures.org/case-study/palagnedra-dam-switzerland-1978/ Learn more about the effect of debris on the spillway at Palagnedra Dam (DamFailures.org)]		{{Website Icon}} [https://damfailures.org/case-study/palagnedra-dam-switzerland-1978/ Learn more about the effect of debris on the spillway at Palagnedra Dam (DamFailures.org)]
	{{Website Icon}} [https://damfailures.org/case-study/spencer-dam-nebraska-2019// Learn more about the effect of ice during the failure of Spencer Dam (DamFailures.org)]		{{Website Icon}} [https://damfailures.org/case-study/spencer-dam-nebraska-2019// Learn more about the effect of ice during the failure of Spencer Dam (DamFailures.org)]

	==Best Practices Resources==		==Best Practices Resources==
	{{Document Icon}} [[Ice Engineering (EM 1110-2-1612)\|Ice Engineering (EM 1110-2-1612) ~~(U.S. Army Corps of Engineers)~~]]		{{Document Icon}} [[Ice Engineering (EM 1110-2-1612)\|Ice Engineering (EM 1110-2-1612), USACE, 2002]]
	{{Document Icon}} [[Ice Pressure on Engineering Structures (CRREL III-B1b)\|Ice Pressure on Engineering Structures (CRREL III-B1b) ~~(U.S. Army Corps of Engineers)~~]]		{{Document Icon}} [[Ice Pressure on Engineering Structures (CRREL III-B1b)\|Ice Pressure on Engineering Structures (CRREL III-B1b), USACE, 1970]]


	<!-- For information on notation for in text citations visit https://www.mediawiki.org/wiki/Help:Cite Or simply enclose the citation as shown <ref> citation </ref> in the location of the in text mention. Citations will automatically populate below-->		<!-- For information on notation for in text citations visit https://www.mediawiki.org/wiki/Help:Cite Or simply enclose the citation as shown <ref> citation </ref> in the location of the in text mention. Citations will automatically populate below-->

Grichards at 03:49, 13 December 2022

2022-12-13T03:49:03Z

← Older revision		Revision as of 03:49, 13 December 2022
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	==Effects of ice on gate structures==		==Effects of ice on gate structures==
	“Dam gates are particularly susceptible to freezing in place because of leaking seals and resulting ice buildup, especially if gates are moved infrequently. Hoisting chains, trunnion arms, etc., may become so loaded with ice a to be too heavy for lifting mechanisms”.<ref name="EM 1110-2-1612" />		“Dam gates are particularly susceptible to freezing in place because of leaking seals and resulting ice buildup, especially if gates are moved infrequently. Hoisting chains, trunnion arms, etc., may become so loaded with ice to be too heavy for lifting mechanisms”.<ref name="EM 1110-2-1612" />

	==Effects of ice on river stage and discharge:==		==Effects of ice on river stage and discharge:==
	“A stationary river ice cover, whether an ice sheet or a jam, introduces an additional boundary and therefore increases energy losses. This translates to an increase in stage compared to open-water conditions for the same discharge. Numerical models for river [[hydraulics]] must be able to account for the effects of ice if they are to reliably describe river flows and stages. The resistance offered by an ice cover will lead to upstream water storage, resulting in rapid stage rise and possible flooding, and simultaneously will lead to a drop in stage and a discharge deficit downstream from the ice cover. If the stage drop is severe enough, downstream water intakes may become ~~exposes~~, affecting municipal and industrial water supplies, especially during periods of drought or very low flow”.<ref name="EM 1110-2-1612" />		“A stationary river ice cover, whether an ice sheet or a jam, introduces an additional boundary and therefore increases energy losses. This translates to an increase in stage compared to open-water conditions for the same discharge. Numerical models for river [[hydraulics]] must be able to account for the effects of ice if they are to reliably describe river flows and stages. The resistance offered by an ice cover will lead to upstream water storage, resulting in rapid stage rise and possible flooding, and simultaneously will lead to a drop in stage and a discharge deficit downstream from the ice cover. If the stage drop is severe enough, downstream water intakes may become exposed, affecting municipal and industrial water supplies, especially during periods of drought or very low flow”.<ref name="EM 1110-2-1612" />

	==Effects of ice on sediment transport and scour==		==Effects of ice on sediment transport and scour==
	“The presence of a floating ice cover roughly doubles the wetted perimeter of a wide channel, which in turn modifies the magnitude and distribution of the velocities and, thus, the boundary and internal shear stresses. For a movable bed channel, an ice cover may, therefore, affect the bed sediment transport and the suspended sediment transport characteristics of the stream and modify the channel geometry and the bed regime. For an abrupt thickening of an ice accumulation, such as the toe of an ice jam, there may be significant bed ~~scout~~ because of the deflection of the flow against the bed. When this happens in the vicinity of a riverine structure, such as a bridge pier, the resulting scour may eventually cause [[structural]] failure”.<ref name="EM 1110-2-1612" />		“The presence of a floating ice cover roughly doubles the wetted perimeter of a wide channel, which in turn modifies the magnitude and distribution of the velocities and, thus, the boundary and internal shear stresses. For a movable bed channel, an ice cover may, therefore, affect the bed sediment transport and the suspended sediment transport characteristics of the stream and modify the channel geometry and the bed regime. For an abrupt thickening of an ice accumulation, such as the toe of an ice jam, there may be significant bed scour because of the deflection of the flow against the bed. When this happens in the vicinity of a riverine structure, such as a bridge pier, the resulting scour may eventually cause [[structural]] failure”.<ref name="EM 1110-2-1612" />

	==Effects of flooding caused by ice jams==		==Effects of flooding caused by ice jams==

Grichards at 03:46, 13 December 2022

2022-12-13T03:46:39Z

← Older revision		Revision as of 03:46, 13 December 2022
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	==Effects of ice on gate structures==		==Effects of ice on gate structures==
	:“Dam gates are particularly susceptible to freezing in place because of leaking seals and resulting ice buildup, especially if gates are moved infrequently. Hoisting chains, trunnion arms, etc., may become so loaded with ice a to be too heavy for lifting mechanisms”.<ref name="EM 1110-2-1612" />		“Dam gates are particularly susceptible to freezing in place because of leaking seals and resulting ice buildup, especially if gates are moved infrequently. Hoisting chains, trunnion arms, etc., may become so loaded with ice a to be too heavy for lifting mechanisms”.<ref name="EM 1110-2-1612" />

	==Effects of ice on river stage and discharge:==		==Effects of ice on river stage and discharge:==
	:“A stationary river ice cover, whether an ice sheet or a jam, introduces an additional boundary and therefore increases energy losses. This translates to an increase in stage compared to open-water conditions for the same discharge. Numerical models for river [[hydraulics]] must be able to account for the effects of ice if they are to reliably describe river flows and stages. The resistance offered by an ice cover will lead to upstream water storage, resulting in rapid stage rise and possible flooding, and simultaneously will lead to a drop in stage and a discharge deficit downstream from the ice cover. If the stage drop is severe enough, downstream water intakes may become exposes, affecting municipal and industrial water supplies, especially during periods of drought or very low flow”.<ref name="EM 1110-2-1612" />		“A stationary river ice cover, whether an ice sheet or a jam, introduces an additional boundary and therefore increases energy losses. This translates to an increase in stage compared to open-water conditions for the same discharge. Numerical models for river [[hydraulics]] must be able to account for the effects of ice if they are to reliably describe river flows and stages. The resistance offered by an ice cover will lead to upstream water storage, resulting in rapid stage rise and possible flooding, and simultaneously will lead to a drop in stage and a discharge deficit downstream from the ice cover. If the stage drop is severe enough, downstream water intakes may become exposes, affecting municipal and industrial water supplies, especially during periods of drought or very low flow”.<ref name="EM 1110-2-1612" />

	==Effects of ice on sediment transport and scour==		==Effects of ice on sediment transport and scour==
	:“The presence of a floating ice cover roughly doubles the wetted perimeter of a wide channel, which in turn modifies the magnitude and distribution of the velocities and, thus, the boundary and internal shear stresses. For a movable bed channel, an ice cover may, therefore, affect the bed sediment transport and the suspended sediment transport characteristics of the stream and modify the channel geometry and the bed regime. For an abrupt thickening of an ice accumulation, such as the toe of an ice jam, there may be significant bed scout because of the deflection of the flow against the bed. When this happens in the vicinity of a riverine structure, such as a bridge pier, the resulting scour may eventually cause [[structural]] failure”.<ref name="EM 1110-2-1612" />		“The presence of a floating ice cover roughly doubles the wetted perimeter of a wide channel, which in turn modifies the magnitude and distribution of the velocities and, thus, the boundary and internal shear stresses. For a movable bed channel, an ice cover may, therefore, affect the bed sediment transport and the suspended sediment transport characteristics of the stream and modify the channel geometry and the bed regime. For an abrupt thickening of an ice accumulation, such as the toe of an ice jam, there may be significant bed scout because of the deflection of the flow against the bed. When this happens in the vicinity of a riverine structure, such as a bridge pier, the resulting scour may eventually cause [[structural]] failure”.<ref name="EM 1110-2-1612" />

	==Effects of flooding caused by ice jams==		==Effects of flooding caused by ice jams==
	:“River ice jams may <noautolinks>contribute</noautolinks> to winter and early spring flood damage. Ice blockages in main stems and tributaries cause stages to rise and force water out of the channel over the [[floodplain]], even when discharges are low compared to warm-water floods. Ice jam floods, while usually not as extensive as open-water floods, often take place with little or no warning. The factors and relationships that determine the probability of ice jams and ice jam flooding are more complex than those for open-water flooding. This means that the extensive statistical analysis methods applied to normal flooding phenomena are not readily applicable to ice-related occurrences. Many mitigation measures have been developed for preventing or reducing ice jam floods; these methods may be structural or nonstructural, and they may be deployed on a permanent, advance, or emergency basis”.<ref name="EM 1110-2-1612" />		“River ice jams may <noautolinks>contribute</noautolinks> to winter and early spring flood damage. Ice blockages in main stems and tributaries cause stages to rise and force water out of the channel over the [[floodplain]], even when discharges are low compared to warm-water floods. Ice jam floods, while usually not as extensive as open-water floods, often take place with little or no warning. The factors and relationships that determine the probability of ice jams and ice jam flooding are more complex than those for open-water flooding. This means that the extensive statistical analysis methods applied to normal flooding phenomena are not readily applicable to ice-related occurrences. Many mitigation measures have been developed for preventing or reducing ice jam floods; these methods may be structural or nonstructural, and they may be deployed on a permanent, advance, or emergency basis”.<ref name="EM 1110-2-1612" />

	==Examples==		==Examples==

Grichards at 03:45, 13 December 2022

2022-12-13T03:45:55Z

← Older revision		Revision as of 03:45, 13 December 2022
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	\| [[Image:Palagnedra2.png\|350px\|x350px\|link=https://damfailures.org/case-study/palagnedra-dam-switzerland-1978/]]		\| [[Image:Palagnedra2.png\|350px\|x350px\|link=https://damfailures.org/case-study/palagnedra-dam-switzerland-1978/]]
	\|-		\|-
	\|style="text-align:center; font-size:90%;"\| Learn more [[about]] the impact of debris on the spillway at [https://damfailures.org/case-study/palagnedra-dam-switzerland-1978/ Palagnedra Dam (DamFailures.org)]		\|style="text-align:center; font-size:90%;"\| Learn more about the impact of debris on the spillway at [https://damfailures.org/case-study/palagnedra-dam-switzerland-1978/ Palagnedra Dam (DamFailures.org)]
	\|}		\|}

Grichards at 03:45, 13 December 2022

2022-12-13T03:45:24Z

← Older revision		Revision as of 03:45, 13 December 2022
Line 9:		Line 9:

	<!-- Delete any sections that are not necessary to your topic. Add pictures/sections as needed -->		<!-- Delete any sections that are not necessary to your topic. Add pictures/sections as needed -->
	“Each year, ice grows on and disappears from the nation’s rivers and lakes in tune with cycles of nature. Unless the ice causes problems, such as flooding or blocking the arteries of commerce, few people pay more than cursory attention. Because of this, the very great variety of ways in which ice initially forms, grows, and ~~accumulated~~, and finally disappears, are relatively unknown. Ice processes on lakes are different from those on rivers, and for both lakes and rivers, the size of the water body affects which processes take place. Ice owes its existence to the thermal process of heat transfer, but is evolution is greatly influenced by physical and mechanical processes”.<ref name="EM 1110-2-1612">[[Ice Engineering (EM 1110-2-1612) \| EM 1110-2-1612 Ice Engineering, USACE, 2002]]</ref>		“Each year, ice grows on and disappears from the nation’s rivers and lakes in tune with cycles of nature. Unless the ice causes problems, such as flooding or blocking the arteries of commerce, few people pay more than cursory attention. Because of this, the very great variety of ways in which ice initially forms, grows, and accumulates, and finally disappears, are relatively unknown. Ice processes on lakes are different from those on rivers, and for both lakes and rivers, the size of the water body affects which processes take place. Ice owes its existence to the thermal process of heat transfer, but its evolution is greatly influenced by physical and mechanical processes”.<ref name="EM 1110-2-1612">[[Ice Engineering (EM 1110-2-1612) \| EM 1110-2-1612 Ice Engineering, USACE, 2002]]</ref>

	The formation, movement, and accumulation of ice in rivers and [[reservoirs]] at, or around, various hydraulic structures complicates the methods used to predict flooding, sediment transport, and scour, as well as complicates the [[operation]] and maintenance of different components of hydraulic structures such as gates, culverts, and bridges.		The formation, movement, and accumulation of ice in rivers and [[reservoirs]] at, or around, various hydraulic structures complicates the methods used to predict flooding, sediment transport, and scour, as well as complicates the [[operation]] and maintenance of different components of hydraulic structures such as gates, culverts, and bridges.

	~~'''~~Effects of ice on gate structures~~:'''~~		==Effects of ice on gate structures==

	:“Dam gates are particularly susceptible to freezing in place because of leaking seals and resulting ice buildup, especially if gates are moved infrequently. Hoisting chains, trunnion arms, etc., may become so loaded with ice a to be too heavy for lifting mechanisms”.<ref name="EM 1110-2-1612" />		:“Dam gates are particularly susceptible to freezing in place because of leaking seals and resulting ice buildup, especially if gates are moved infrequently. Hoisting chains, trunnion arms, etc., may become so loaded with ice a to be too heavy for lifting mechanisms”.<ref name="EM 1110-2-1612" />

	~~'''~~Effects of ice on river stage and discharge:~~'''~~		==Effects of ice on river stage and discharge:==

	:“A stationary river ice cover, whether an ice sheet or a jam, introduces an additional boundary and therefore increases energy losses. This translates to an increase in stage compared to open-water conditions for the same discharge. Numerical models for river [[hydraulics]] must be able to account for the effects of ice if they are to reliably describe river flows and stages. The resistance offered by an ice cover will lead to upstream water storage, resulting in rapid stage rise and possible flooding, and simultaneously will lead to a drop in stage and a discharge deficit downstream from the ice cover. If the stage drop is severe enough, downstream water intakes may become exposes, affecting municipal and industrial water supplies, especially during periods of drought or very low flow”.<ref name="EM 1110-2-1612" />		:“A stationary river ice cover, whether an ice sheet or a jam, introduces an additional boundary and therefore increases energy losses. This translates to an increase in stage compared to open-water conditions for the same discharge. Numerical models for river [[hydraulics]] must be able to account for the effects of ice if they are to reliably describe river flows and stages. The resistance offered by an ice cover will lead to upstream water storage, resulting in rapid stage rise and possible flooding, and simultaneously will lead to a drop in stage and a discharge deficit downstream from the ice cover. If the stage drop is severe enough, downstream water intakes may become exposes, affecting municipal and industrial water supplies, especially during periods of drought or very low flow”.<ref name="EM 1110-2-1612" />

	~~'''~~Effects of ice on sediment transport and scour~~:'''~~		==Effects of ice on sediment transport and scour==

	:“The presence of a floating ice cover roughly doubles the wetted perimeter of a wide channel, which in turn modifies the magnitude and distribution of the velocities and, thus, the boundary and internal shear stresses. For a movable bed channel, an ice cover may, therefore, affect the bed sediment transport and the suspended sediment transport characteristics of the stream and modify the channel geometry and the bed regime. For an abrupt thickening of an ice accumulation, such as the toe of an ice jam, there may be significant bed scout because of the deflection of the flow against the bed. When this happens in the vicinity of a riverine structure, such as a bridge pier, the resulting scour may eventually cause [[structural]] failure”.<ref name="EM 1110-2-1612" />		:“The presence of a floating ice cover roughly doubles the wetted perimeter of a wide channel, which in turn modifies the magnitude and distribution of the velocities and, thus, the boundary and internal shear stresses. For a movable bed channel, an ice cover may, therefore, affect the bed sediment transport and the suspended sediment transport characteristics of the stream and modify the channel geometry and the bed regime. For an abrupt thickening of an ice accumulation, such as the toe of an ice jam, there may be significant bed scout because of the deflection of the flow against the bed. When this happens in the vicinity of a riverine structure, such as a bridge pier, the resulting scour may eventually cause [[structural]] failure”.<ref name="EM 1110-2-1612" />

	~~'''~~Effects of flooding caused by ice jams~~:'''~~		==Effects of flooding caused by ice jams==
			:“River ice jams may <noautolinks>contribute</noautolinks> to winter and early spring flood damage. Ice blockages in main stems and tributaries cause stages to rise and force water out of the channel over the [[floodplain]], even when discharges are low compared to warm-water floods. Ice jam floods, while usually not as extensive as open-water floods, often take place with little or no warning. The factors and relationships that determine the probability of ice jams and ice jam flooding are more complex than those for open-water flooding. This means that the extensive statistical analysis methods applied to normal flooding phenomena are not readily applicable to ice-related occurrences. Many mitigation measures have been developed for preventing or reducing ice jam floods; these methods may be structural or nonstructural, and they may be deployed on a permanent, advance, or emergency basis”.<ref name="EM 1110-2-1612" />
	:“River ice jams may <noautolinks>contribute</noautolinks> to winter and early spring flood damage. Ice blockages in main stems and tributaries cause stages to rise and force water out of the channel over the floodplain, even when discharges are low compared to warm-water floods. Ice jam floods, while usually not as extensive as open-water floods, often take place with little or no warning. The factors and relationships that determine the probability of ice jams and ice jam flooding are more complex than those for open-water flooding. This means that the extensive statistical analysis methods applied to normal flooding phenomena are not readily applicable to ice-related occurrences. Many mitigation measures have been developed for preventing or reducing ice jam floods; these methods may be structural or nonstructural, and they may be deployed on a permanent, advance, or emergency basis”.<ref name="EM 1110-2-1612" />

	~~'''Ice loads on structures:'''~~

	~~:[Paragraph here]~~

	~~'''Expanding reservoir ice load structures:'''~~

	~~:[Paragraph here]~~

	~~'''Dynamic ice load on structures:'''~~

	~~:[Paragraph here]~~

	==Examples==		==Examples==

Grichards at 21:44, 9 December 2022

2022-12-09T21:44:00Z

← Older revision		Revision as of 21:44, 9 December 2022
Line 27:		Line 27:
	'''Effects of flooding caused by ice jams:'''		'''Effects of flooding caused by ice jams:'''

	:“River ice jams may <noautolinks>[[contribute]]<noautolinks/> to winter and early spring flood damage. Ice blockages in main stems and tributaries cause stages to rise and force water out of the channel over the floodplain, even when discharges are low compared to warm-water floods. Ice jam floods, while usually not as extensive as open-water floods, often take place with little or no warning. The factors and relationships that determine the probability of ice jams and ice jam flooding are more complex than those for open-water flooding. This means that the extensive statistical analysis methods applied to normal flooding phenomena are not readily applicable to ice-related occurrences. Many mitigation measures have been developed for preventing or reducing ice jam floods; these methods may be structural or nonstructural, and they may be deployed on a permanent, advance, or emergency basis”.<ref name="EM 1110-2-1612" />		:“River ice jams may <noautolinks>contribute</noautolinks> to winter and early spring flood damage. Ice blockages in main stems and tributaries cause stages to rise and force water out of the channel over the floodplain, even when discharges are low compared to warm-water floods. Ice jam floods, while usually not as extensive as open-water floods, often take place with little or no warning. The factors and relationships that determine the probability of ice jams and ice jam flooding are more complex than those for open-water flooding. This means that the extensive statistical analysis methods applied to normal flooding phenomena are not readily applicable to ice-related occurrences. Many mitigation measures have been developed for preventing or reducing ice jam floods; these methods may be structural or nonstructural, and they may be deployed on a permanent, advance, or emergency basis”.<ref name="EM 1110-2-1612" />

	'''Ice loads on structures:'''		'''Ice loads on structures:'''

Grichards at 21:42, 9 December 2022

2022-12-09T21:42:57Z

← Older revision		Revision as of 21:42, 9 December 2022
Line 27:		Line 27:
	'''Effects of flooding caused by ice jams:'''		'''Effects of flooding caused by ice jams:'''

	:“River ice jams may [[contribute]] to winter and early spring flood damage. Ice blockages in main stems and tributaries cause stages to rise and force water out of the channel over the floodplain, even when discharges are low compared to warm-water floods. Ice jam floods, while usually not as extensive as open-water floods, often take place with little or no warning. The factors and relationships that determine the probability of ice jams and ice jam flooding are more complex than those for open-water flooding. This means that the extensive statistical analysis methods applied to normal flooding phenomena are not readily applicable to ice-related occurrences. Many [[mitigation]] measures have been developed for preventing or reducing ice jam floods; these methods may be structural or nonstructural, and they may be deployed on a permanent, advance, or emergency basis”.<ref name="EM 1110-2-1612" />		:“River ice jams may <noautolinks>[[contribute]]<noautolinks/> to winter and early spring flood damage. Ice blockages in main stems and tributaries cause stages to rise and force water out of the channel over the floodplain, even when discharges are low compared to warm-water floods. Ice jam floods, while usually not as extensive as open-water floods, often take place with little or no warning. The factors and relationships that determine the probability of ice jams and ice jam flooding are more complex than those for open-water flooding. This means that the extensive statistical analysis methods applied to normal flooding phenomena are not readily applicable to ice-related occurrences. Many mitigation measures have been developed for preventing or reducing ice jam floods; these methods may be structural or nonstructural, and they may be deployed on a permanent, advance, or emergency basis”.<ref name="EM 1110-2-1612" />

	'''Ice loads on structures:'''		'''Ice loads on structures:'''

Grichards at 05:03, 18 November 2022

2022-11-18T05:03:53Z

Grichards at 03:07, 17 September 2022

2022-09-17T03:07:20Z

← Older revision		Revision as of 03:07, 17 September 2022
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	__NOTOC__		__NOTOC__
	----		----
			{\| align="right" style="width:10%;" cellpadding="7"
			\| [[Image:Palagnedra2.png\|350px\|x350px\|link=https://damfailures.org/case-study/palagnedra-dam-switzerland-1978/]]
			\|-
			\|style="text-align:center; font-size:90%;"\| Learn more about the impact of debris on the spillway at [https://damfailures.org/case-study/palagnedra-dam-switzerland-1978/ Palagnedra Dam (DamFailures.org)]
			\|}

	<!-- Delete any sections that are not necessary to your topic. Add pictures/sections as needed -->		<!-- Delete any sections that are not necessary to your topic. Add pictures/sections as needed -->
	“Each year, ice grows on and disappears from the nation’s rivers and lakes in tune with cycles of nature. Unless the ice causes problems, such as flooding or blocking the arteries of commerce, few people pay more than cursory attention. Because of this, the very great variety of ways in which ice initially forms, grows, and accumulated, and finally disappears, are relatively unknown. Ice processes on lakes are different from those on rivers, and for both lakes and rivers, the size of the water body affects which processes take place. Ice owes its existence to the thermal process of heat transfer, but is evolution is greatly influenced by physical and mechanical processes”.<ref name="EM 1110-2-1612">[[Ice Engineering (EM 1110-2-1612) \| EM 1110-2-1612 Ice Engineering, USACE, 2002]]</ref>		“Each year, ice grows on and disappears from the nation’s rivers and lakes in tune with cycles of nature. Unless the ice causes problems, such as flooding or blocking the arteries of commerce, few people pay more than cursory attention. Because of this, the very great variety of ways in which ice initially forms, grows, and accumulated, and finally disappears, are relatively unknown. Ice processes on lakes are different from those on rivers, and for both lakes and rivers, the size of the water body affects which processes take place. Ice owes its existence to the thermal process of heat transfer, but is evolution is greatly influenced by physical and mechanical processes”.<ref name="EM 1110-2-1612">[[Ice Engineering (EM 1110-2-1612) \| EM 1110-2-1612 Ice Engineering, USACE, 2002]]</ref>
Line 35:		Line 41:

	==Examples==		==Examples==
	{{Website Icon}}		{{Website Icon}} [https://damfailures.org/case-study/palagnedra-dam-switzerland-1978/ Learn more about the effect of debris on the spillway at Palagnedra Dam (DamFailures.org)]
			{{Website Icon}} [https://damfailures.org/case-study/spencer-dam-nebraska-2019// Learn more about the effect of ice during the failure of Spencer Dam (DamFailures.org)]
	==Best Practices Resources==		==Best Practices Resources==
	{{Document Icon}} [[Ice Engineering (EM 1110-2-1612)]]		{{Document Icon}} [[Ice Engineering (EM 1110-2-1612)\|Ice Engineering (EM 1110-2-1612) (U.S. Army Corps of Engineers)]]
	~~==Trainings==~~		{{Document Icon}} [[Ice Pressure on Engineering Structures (CRREL III-B1b)\|Ice Pressure on Engineering Structures (CRREL III-B1b) (U.S. Army Corps of Engineers)]]
	{{~~Video~~ Icon}}

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← Older revision		Revision as of 05:03, 18 November 2022
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			[[Category:Flood]]
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	{\| align="right" style="width:10%;" cellpadding="7"		{\| align="right" style="width:10%;" cellpadding="7"
	\| [[Image:Palagnedra2.png\|350px\|x350px\|link=https://damfailures.org/case-study/palagnedra-dam-switzerland-1978/]]		\| [[Image:Palagnedra2.png\|350px\|x350px\|link=https://damfailures.org/case-study/palagnedra-dam-switzerland-1978/]]
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	\|style="text-align:center; font-size:90%;"\| Learn more about the impact of debris on the spillway at [https://damfailures.org/case-study/palagnedra-dam-switzerland-1978/ Palagnedra Dam (DamFailures.org)]		\|style="text-align:center; font-size:90%;"\| Learn more [[about]] the impact of debris on the spillway at [https://damfailures.org/case-study/palagnedra-dam-switzerland-1978/ Palagnedra Dam (DamFailures.org)]
	\|}		\|}

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	“Each year, ice grows on and disappears from the nation’s rivers and lakes in tune with cycles of nature. Unless the ice causes problems, such as flooding or blocking the arteries of commerce, few people pay more than cursory attention. Because of this, the very great variety of ways in which ice initially forms, grows, and accumulated, and finally disappears, are relatively unknown. Ice processes on lakes are different from those on rivers, and for both lakes and rivers, the size of the water body affects which processes take place. Ice owes its existence to the thermal process of heat transfer, but is evolution is greatly influenced by physical and mechanical processes”.<ref name="EM 1110-2-1612">[[Ice Engineering (EM 1110-2-1612) \| EM 1110-2-1612 Ice Engineering, USACE, 2002]]</ref>		“Each year, ice grows on and disappears from the nation’s rivers and lakes in tune with cycles of nature. Unless the ice causes problems, such as flooding or blocking the arteries of commerce, few people pay more than cursory attention. Because of this, the very great variety of ways in which ice initially forms, grows, and accumulated, and finally disappears, are relatively unknown. Ice processes on lakes are different from those on rivers, and for both lakes and rivers, the size of the water body affects which processes take place. Ice owes its existence to the thermal process of heat transfer, but is evolution is greatly influenced by physical and mechanical processes”.<ref name="EM 1110-2-1612">[[Ice Engineering (EM 1110-2-1612) \| EM 1110-2-1612 Ice Engineering, USACE, 2002]]</ref>

	The formation, movement, and accumulation of ice in rivers and reservoirs at, or around, various hydraulic structures complicates the methods used to predict flooding, sediment transport, and scour, as well as complicates the operation and maintenance of different components of hydraulic structures such as gates, culverts, and bridges.		The formation, movement, and accumulation of ice in rivers and [[reservoirs]] at, or around, various hydraulic structures complicates the methods used to predict flooding, sediment transport, and scour, as well as complicates the [[operation]] and maintenance of different components of hydraulic structures such as gates, culverts, and bridges.

	'''Effects of ice on gate structures:'''		'''Effects of ice on gate structures:'''
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	'''Effects of ice on river stage and discharge:'''		'''Effects of ice on river stage and discharge:'''

	:“A stationary river ice cover, whether an ice sheet or a jam, introduces an additional boundary and therefore increases energy losses. This translates to an increase in stage compared to open-water conditions for the same discharge. Numerical models for river hydraulics must be able to account for the effects of ice if they are to reliably describe river flows and stages. The resistance offered by an ice cover will lead to upstream water storage, resulting in rapid stage rise and possible flooding, and simultaneously will lead to a drop in stage and a discharge deficit downstream from the ice cover. If the stage drop is severe enough, downstream water intakes may become exposes, affecting municipal and industrial water supplies, especially during periods of drought or very low flow”.<ref name="EM 1110-2-1612" />		:“A stationary river ice cover, whether an ice sheet or a jam, introduces an additional boundary and therefore increases energy losses. This translates to an increase in stage compared to open-water conditions for the same discharge. Numerical models for river [[hydraulics]] must be able to account for the effects of ice if they are to reliably describe river flows and stages. The resistance offered by an ice cover will lead to upstream water storage, resulting in rapid stage rise and possible flooding, and simultaneously will lead to a drop in stage and a discharge deficit downstream from the ice cover. If the stage drop is severe enough, downstream water intakes may become exposes, affecting municipal and industrial water supplies, especially during periods of drought or very low flow”.<ref name="EM 1110-2-1612" />

	'''Effects of ice on sediment transport and scour:'''		'''Effects of ice on sediment transport and scour:'''

	:“The presence of a floating ice cover roughly doubles the wetted perimeter of a wide channel, which in turn modifies the magnitude and distribution of the velocities and, thus, the boundary and internal shear stresses. For a movable bed channel, an ice cover may, therefore, affect the bed sediment transport and the suspended sediment transport characteristics of the stream and modify the channel geometry and the bed regime. For an abrupt thickening of an ice accumulation, such as the toe of an ice jam, there may be significant bed scout because of the deflection of the flow against the bed. When this happens in the vicinity of a riverine structure, such as a bridge pier, the resulting scour may eventually cause structural failure”.<ref name="EM 1110-2-1612" />		:“The presence of a floating ice cover roughly doubles the wetted perimeter of a wide channel, which in turn modifies the magnitude and distribution of the velocities and, thus, the boundary and internal shear stresses. For a movable bed channel, an ice cover may, therefore, affect the bed sediment transport and the suspended sediment transport characteristics of the stream and modify the channel geometry and the bed regime. For an abrupt thickening of an ice accumulation, such as the toe of an ice jam, there may be significant bed scout because of the deflection of the flow against the bed. When this happens in the vicinity of a riverine structure, such as a bridge pier, the resulting scour may eventually cause [[structural]] failure”.<ref name="EM 1110-2-1612" />

	'''Effects of flooding caused by ice jams:'''		'''Effects of flooding caused by ice jams:'''

	:“River ice jams may contribute to winter and early spring flood damage. Ice blockages in main stems and tributaries cause stages to rise and force water out of the channel over the floodplain, even when discharges are low compared to warm-water floods. Ice jam floods, while usually not as extensive as open-water floods, often take place with little or no warning. The factors and relationships that determine the probability of ice jams and ice jam flooding are more complex than those for open-water flooding. This means that the extensive statistical analysis methods applied to normal flooding phenomena are not readily applicable to ice-related occurrences. Many mitigation measures have been developed for preventing or reducing ice jam floods; these methods may be structural or nonstructural, and they may be deployed on a permanent, advance, or emergency basis”.<ref name="EM 1110-2-1612" />		:“River ice jams may [[contribute]] to winter and early spring flood damage. Ice blockages in main stems and tributaries cause stages to rise and force water out of the channel over the floodplain, even when discharges are low compared to warm-water floods. Ice jam floods, while usually not as extensive as open-water floods, often take place with little or no warning. The factors and relationships that determine the probability of ice jams and ice jam flooding are more complex than those for open-water flooding. This means that the extensive statistical analysis methods applied to normal flooding phenomena are not readily applicable to ice-related occurrences. Many [[mitigation]] measures have been developed for preventing or reducing ice jam floods; these methods may be structural or nonstructural, and they may be deployed on a permanent, advance, or emergency basis”.<ref name="EM 1110-2-1612" />

	'''Ice loads on structures:'''		'''Ice loads on structures:'''