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Dy= (W +(Dx)^2/v)sin () where: w= angular velocity Dx= distance traveled v- velocity l= latitude |
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Couloumb- Terghazi Failure Criterion |
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s= c + (p- Hw)tan(failure angle)
c= cohesion p= pressure on soil load Hw= pressure of water failure angle= yea duh |
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KE= 1/2mass x velocity^2
The shapes and depth of crater is determined by the kinestic energy of impactor and type of crust that it impacts |
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9.1 magnitude with foreshocks and aftershocks. - Subduction zone lead to tsunami, as well as subducting of plates to make the land more vulnerable. |
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Volcano warnings: - gas releases - seismic readings show that there was movement and stress was building - displacements in land - There was evacuation |
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Washington 1980 Stratovolcano- felsic had a caldera, which clogged it. And the earthquake blew it out and caused pyroclastic flow |
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Loma Prieta Earthquake- San Andres |
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7.1 magnitude caused liquefzction and base amplification |
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Sumatra Tsunami- Indonesia- 2004 |
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Definition
caused by a subducting plate triggering an earthquake. The tsunami killed thousands in 14 countries. magnitude of 91.-9.3 |
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Hazards- storm surge, rain - not worst case scenario: hit east of NOLA - Levees built for CAT 3 failed (overtopped and pushed out) - destroyed wetlands |
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Cat 2 Massively exposed population in dense city (persistent rainfall) - slow movement had sustained winds and rain - storm surge (Jersey shore) - lifeloss was comparable to that of 1994 Northridge earthquake |
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Strange path: formed in Carribean, started in North but veered west toward central america - Stalled in honduras, CAT 5, - Huge flooding and mudslides - killed around 10,000 |
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measure of explosivity of a volcano -gauge of the volume, height - quantative - 1-8 |
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-silica content - volatiles - viscosity |
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4 types of landslide movements |
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Definition
- falls - slides - subsides - flows |
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Rotational: driving force vs. resisting force Translational: -CREEP (expansion and contraction) - sliding along a point of weakness (joint, fault) |
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loosely packed soil limestone dissolves |
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couloumb failure criteria |
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Definition
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water's effect on slope stablilty |
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Definition
- weight - makes soil less cohesive - decrease in friciton - air hockey table effect- increasing shear stress |
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Definition
- hard to forcast - try to look at types of soil, moisture, topography |
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Definition
we have it because in the Troposphere, the warm air is below the cold air, leading to instability |
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Abiabatic cooling and heating |
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Definition
this fuels storms happens when there is a phase change for air and moisture. - when air rises, it cools as pressure decreases - it condensates, but this process gives off heat, fueling more rising - The graph shows that this is why moist air is warmer than dry air |
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large scale lateral flow of energy in atmosphere |
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Definition
- ALBEDO- relfection - the low latitudes transfer heat to the higher latitudes - Also pressure radiants changes over seasons |
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Cumulous- large puffy, dense, stormy Stratus- large gray, dense, precipitationm cirrus- high and whispy |
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- happens in low pressure systems because vapor consensates |
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early stage: warm water causes upwelling and cloud formation middle stage: low pressure causes condensation and precipitation (downwelling) end stage: downwelling chokes out the upwelling |
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Tornadoes - they occur when a cell forms but is pushed to the side by a wind (jet stream) - large, rotating updraft (tornado) - clouds are sheared by winds - asymetry causes rotation |
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conservation of angular momentum |
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Definition
used for tornadoes and hurricanes - describes the behavior of a spinning mass - Decreasing the radium of an object will increase its velocity |
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happens in this region due to the meeting of warm and cold air - sometimes the warm air gets stuck under the cold air in a low pressure system and the jet stream pushes the cell to make a tornado |
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- massive "mesocyclone" that is rotation due to coriolus force. - the storm is fueled by warm oceans, and pushed west in the northern hemisphere by trade winds. |
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Definition
- has to do with adiabatic heating and cooling - when moist air is rising and then condenses,latent heat is released from the phase change, allowing for more rising and fuel for hurricane |
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Coriolus force (explanation) |
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Definition
- deflection of objects relative to a rotating reference - higher velocity, lower the coriolus force - lower the velocity, higher the coliolus force |
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- starts are tropical disturbance formed in low pressure systems - fueled as it moves west by trade winds, over warm ocean. - warm ocean fuels the upwelling of the hurricane - forms at low latitudes, because of Albedo - coriolus force makes it spin counter clockwise in the northern hemisphere |
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Saffer- Simpson Intensity scale for Hurricanes |
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Definition
1-5 categories. 5 has low pressure, alot of wind, and storm surge. - mostly empirical |
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Forecasting and Tracking hurricanes |
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Definition
- prediction of the storm can be done by tracking the wind, storm surges, temperature of water, rain - forecasting precursory conditions - satelites and doppler radar - pressure guages |
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Challenges of forecasting and Tracking hurricanes |
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Definition
- evacuation is hard - dont have enough time for evac |
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flash: happen quickly, can take many lives, dont do as much damage as regional floods Regional: floods that happen slowly, and stay for a while in a drainage basin. They can destroy cities. caused by rainfall |
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if you drop water, it will flow to here |
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normally sea level. where there is no more eroding in the river |
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area that the water occupies in a river if the water level is high |
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the turning of a river slows it down. normally happens in the low lands |
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forecasting floods- long term, and tools |
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long term: - knowledge of topography, sinuosity, shape of rivers - basin size and shape - precipitation levels Tools: hydrograph: records discharge level flood frequency curves! |
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Definition
dams, levees/ channels, river restoration, retention ponds, land use planning |
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gases- CO2, NO2 and O-zone - it is good that that o-zone layer keeps the radiant heat in, but human induced greenhouse gases have enhanced greenhouse effect |
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regional impacts on global warming |
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Definition
- severe winter storms - sea level changes - more storms, precip - hurricanes - melting of ice caps - wildfires |
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5 causes of sea level change |
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Definition
- dams influencing water drainage - melting of ice caps - techntonic displacement - warming of ocean water - ocean circulation changes |
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ways of guaging sea level |
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tidal guage- measures sea level at certain area. not good because ocean water is not eustatic satellite altimetery- meansures sea level from space |
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how anomolous is recent sea level change? |
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Definition
it is anomolous. we can see this from the Roman fish pens that water was lower, and from the ancient coral, that the sea level was higher |
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Eustatic sea level change |
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not true. the global sea level varies due to various factors |
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last interglacial period- sea level was 7m higher than it is today |
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merioriod, meteor, metiorite |
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meteoriod: peieces of comet or asteriod meteor: orbits sun meteorite: on track to hit earth |
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oors cloud - where grvitational pull from sun stops |
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yucaton peninsula chixulub structure came from southeast |
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breakdown of chemical structure -> more flammable |
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dry and fast over mountain |
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