Introduction to Atmospheric Dynamics
Introduction to Atmospheric Dynamics
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Відео

The Art of Climate Modeling Lecture 10 - Model Intercomparison and Evaluation
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Model Evaluation Hierarchy; Observational Products; Reanalysis Data; Tools for Model Evaluation
The Art of Climate Modeling Lecture 09b - Parameterizations Part 2
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Parameterizing Microphysics; Parameterizing Radiation; Evaluating and Tuning Parameterizations
The Art of Climate Modeling Lecture 09a - Parameterizations Part 1
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Scales of Parameterization; Parameterizing Turbulence; Parameterizing Convection and Clouds
The Art of Climate Modeling Lecture 08 - Variable Resolution Modeling
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Variable Resolution Models; Applications of Variable Resolution Modeling Systems; Challenges for Variable Resolution Modeling
The Art of Climate Modeling Lecture 07 - Parallelism and Supercomputing
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Supercomputer architectures; Programming models; Applications to global climate modeling
The Art of Climate Modeling Lecture 06 - Diffusion, Filters and Fixers
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Explicit and Implicit Diffusion; Filters; Fixers; Dissipation; Numerical Viscosity; Effects of Diffusion
The Art of Climate Modeling Lecture 05 - Vertical Discretizations
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Differences in discretizing the vertical and horizontal; Equation sets and vertical coordinate systems; Representation of topography in models; Computational modes and vertical staggering
The Art of Climate Modeling Lecture 04b - Temporal Discretizations Part 2
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Runge-Kutta methods; Semi-Lagrangian methods; Stability in the dynamical core
The Art of Climate Modeling Lecture 04a - Temporal Discretizations Part 1
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Converting discrete partial differential equations to ordinary differential equations; explicit and implicit methods; forward Euler method; backward Euler method
The Art of Climate Modeling Lecture 03b - Spatial Discretizations Part 2
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Finite volume methods; spectral transform methods; finite element methods
The Art of Climate Modeling Lecture 03a - Spatial Discretizations Part 1
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The atmospheric dynamical core; choice of grid; numerical issues; finite difference methods; grid staggering
The Art of Climate Modeling Lecture 02 - Overview of CESM
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Overview Community Earth System Model (CESM); CESM configurations
The Art of Climate Modeling Lecture 01 - Overview / History
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What are climate models? History of climate models and numerical weather prediction models
Our Changing Atmosphere Lecture 19 - Climate Justice and Climate Impacts
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Environmental Justice; Climate Justice and Injustice; Climate Change Impacts
Our Changing Atmosphere Lecture 18 - Mitigation and Adaptation
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Our Changing Atmosphere Lecture 18 - Mitigation and Adaptation
Our Changing Atmosphere Lecture 17 - Extreme Storms and Precipitation
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Our Changing Atmosphere Lecture 17 - Extreme Storms and Precipitation
Our Changing Atmosphere Lecture 16 - Extreme Weather in California
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Our Changing Atmosphere Lecture 16 - Extreme Weather in California
Our Changing Atmosphere Lecture 15 - Drought in California
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Our Changing Atmosphere Lecture 15 - Drought in California
Our Changing Atmosphere Lecture 14 - General Circulation and Midlatitudinal Weather
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Our Changing Atmosphere Lecture 14 - General Circulation and Midlatitudinal Weather
Our Changing Atmosphere Lecture 13 - Atmospheric Dynamics
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Our Changing Atmosphere Lecture 13 - Atmospheric Dynamics
Our Changing Atmosphere Lecture 12 - Water in California
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Our Changing Atmosphere Lecture 12 - Water in California
Our Changing Atmosphere Lecture 11 - Clouds and Precipitation
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Our Changing Atmosphere Lecture 11 - Clouds and Precipitation
Our Changing Atmosphere Lecture 10 - Water in the Atmosphere
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Our Changing Atmosphere Lecture 10 - Water in the Atmosphere
Our Changing Atmosphere Lecture 09 - Ozone and the Ozone Hole
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Our Changing Atmosphere Lecture 09 - Ozone and the Ozone Hole
Our Changing Atmosphere Lecture 08 - Aerosols
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Our Changing Atmosphere Lecture 08 - Aerosols
Our Changing Atmosphere Lecture 07 - Global Warming
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Our Changing Atmosphere Lecture 07 - Global Warming
Our Changing Atmosphere Lecture 06 - Energy and the Earth System
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Our Changing Atmosphere Lecture 06 - Energy and the Earth System
Our Changing Atmosphere Lecture 05 - Temperature and Energy
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Our Changing Atmosphere Lecture 05 - Temperature and Energy
Our Changing Atmosphere Lecture 04 - Paleoclimate
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Our Changing Atmosphere Lecture 04 - Paleoclimate

КОМЕНТАРІ

  • @whatabouttheearth
    @whatabouttheearth 27 днів тому

    These are all basically the same question. If the ice melted in the Arctic wouldn't we see a smoothing out of the temperature gradiant across the polar front? And wouldn't the polar easterlies warm, therefore decreasing their density, and therefore weakening upward convection of the ferrel cells warm westerlies that get pushed upward by the cold polar easterlies to make the polar low pressure? So wouldn't warming of the Arctic weaken (possibly severely) the polar cell and the northern part of the ferrel cell?

  • @farukifahim
    @farukifahim 27 днів тому

    Amazing series! Is it possible to share the slides or notes of this series?

  • @damienthorne861
    @damienthorne861 Місяць тому

    Boy I have a lot to learn

  • @damienthorne861
    @damienthorne861 Місяць тому

    I love these videos are awesome they're exactly what I needed

  • @munirahmadnayak7
    @munirahmadnayak7 Місяць тому

    This is great. Can we find the PDFs of the presentations?

  • @elvy036
    @elvy036 Місяць тому

    Thank you so much for this video! Helped me a lot to understand parametrization for my exam :)

  • @denizkaragullu6239
    @denizkaragullu6239 Місяць тому

    You are amazing! Thank you so so much

  • @EternalFootman-kr6yx
    @EternalFootman-kr6yx Місяць тому

    Huh?

  • @joyboyboy
    @joyboyboy 3 місяці тому

    I was with you until you showed the hokey stick. Goodbye.

  • @daveandrews9634
    @daveandrews9634 4 місяці тому

    Even with all that money and computing power the models are still way off.

    • @introductiontoatmosphericd284
      @introductiontoatmosphericd284 4 місяці тому

      I think they do pretty well, considering the complexity of the system. Mean climate statistics have been improving with each generation. The biggest challenges relate mostly to small scale convection (e.g., thunderstorms).

  • @damienthorne861
    @damienthorne861 4 місяці тому

    Omg I love this! I was looking for exactly this!!

  • @catvalentine4317
    @catvalentine4317 5 місяців тому

    Extremely helpful - thank you!!

  • @costrio
    @costrio 7 місяців тому

    "Holy balogna Batman?? IMO, CO2 does not drive temeperature -- it follows it,.

  • @costrio
    @costrio 7 місяців тому

    At 2:23 the image shows variability in tree ring width from side to side. If one is working on an early tree ring sample do they have the full diameter or just "one side" of it, I wonder.

  • @vladkrus5796
    @vladkrus5796 7 місяців тому

    Thanks its helpful to understand the weather climate up to this date 2024

  • @赵昀-r6x
    @赵昀-r6x 8 місяців тому

    Great lesson. Does anyone know why the adjustment rate of the ocean is 15 W m2 K-1? (#6:41)

  • @mahashalatv
    @mahashalatv 8 місяців тому

    Please is there a place where i can solve questions after watching all the videos

  • @kenmerry2729
    @kenmerry2729 10 місяців тому

    I did not hear how you calculate temperature from tree rings? Which I understand is what lead to the "Hockey Stick" using these proxies of prior temperature. These tree rings then in modern day do not match with actual records. Therefore there must be something wrong with the "Hockey Stick" ??

  • @tsehayenegash8394
    @tsehayenegash8394 11 місяців тому

    I have a temperature data, how can I calculate the wave number by using this temperature data? thank you

  • @tsehayenegash8394
    @tsehayenegash8394 11 місяців тому

    Do you have Hovmellor matlab code

  • @maxtabmann6701
    @maxtabmann6701 11 місяців тому

    Thank you for making that clear. Climate modelling is an art and no science.

  • @petarswift5089
    @petarswift5089 11 місяців тому

    History of the climate model? Son, there is no mention of Milankovitch in your school textbooks?! I'm sorry that they condemned you to eternal darkness at such a young age.

  • @Rene-uz3eb
    @Rene-uz3eb 11 місяців тому

    What I want to know is why scientists don't use antarctic ice core data to determine co2 levels beyond 800 000 years ago, when we know the antarctic ice sheet formed 34 million years ago. Only the accuracy of timing beyond 800 000 years is lost, but we still know that since in all the ice core data there wasn't an instance with co2 levels beyond 300ppm, this means there wasn't an elevated co2 level up to 34 millions ago either, contradicting the unreliable proxies. And since we now could adjust the proxies with that information, it would mean the co2 levels were estimated too high even beyond 34 million years ago. Finally, given that crustaceans never all went extinct, since they appeared 500 million years ago, but they can't exist without sufficient carbonate, which is disappearing with the acidification of the oceans right now, that again, we were never in a co2/methane regime like we are now, ever since animal life appeared basically. We can't lose ocean life, that would be terminal I think. So my suggestion would be no more new fossil projects, write off everything that's still in the ground and untapped (until maybe a thousand years later when we feel like preventing an ice age). Make existing production expensive by a phased in massive tax over 10 years, so nobody is going to buy new ice vehicles much longer 22:21 yes I don't buy the linear correlation of O18 with temperature. It's not going to be linear and depend on a bunch of other variables. 27:11 I think it is very dangerous to 'estimate' that co2 was much higher back then based on some random co2 models from a few people. In my mind there is absolutely no way to estimate the turnover in biomass and the amount of biomass that has decomposed back into the atmosphere..I mean seriously go pound sand. All we know about co2 for sure is the antarctic ice core record and that one is clear as hell: do not go over 300 ppm. And yes nobody talks about the sun having been much weaker back then (according to same models I take it) which means you can't take elevated co2 levels at face value. In any case this 'co2 was higher nothing happened' is gaslighting.

  • @ahamill130
    @ahamill130 Рік тому

    Geography teacher from the UK here. This is an excellent video - clear, succinct yet detailed. Very helpful indeed.

  • @yitaoliu1318
    @yitaoliu1318 Рік тому

    Great talk that helps me build general knowledge about the model Intercomparison and evaluation. Thank you a lot!

  • @pulsar22
    @pulsar22 Рік тому

    What is wrong with the feedback loop claimed for CO2? Big question is how then does glacial maxima terminate and how does interglacial terminate if CO2 is a major factor. That CO2 lags both termination means that CO2 concentration is the effect and not the cause. Otherwise, it would either be that we are stuck at warm temperatures or we are stuck at the bottom of a glacial maxima. If ever CO2 has any effects, it is too small to be the driver of global temperature.

    • @DrSmooth2000
      @DrSmooth2000 Рік тому

      Just saw an answer tonight. The 100k and 41k milankovich cycles have to both line up. Creating a double summer.

  • @daveandrews9634
    @daveandrews9634 Рік тому

    Tom Gallagher from Calgary University explains the climate record quite accurately using the continental drift theory and carbonic acid cycle. CO2 doesn’t play any significant roll in his theory but it is quite compelling.

  • @daveandrews9634
    @daveandrews9634 Рік тому

    The CO2 warming theory leaves out the role of carbonic acid in the climate cycle. The other factor missing is the Beryllium-7 paleo data that recorded the suns effect on climate which along with water vapor and clouds explains the climate record quite well. Climate scientists need to remove the CO2 goggles so that they can see the real drivers of climate.

  • @tsehayenegash8394
    @tsehayenegash8394 Рік тому

    What is the meaning of annual oscillation (AO)?

  • @daveandrews9634
    @daveandrews9634 Рік тому

    A couple suggestions: Where is the W/m2 change due to the greening of the earth from CO2 fertilization? There is also no discussion about the decreasing effect of CO2 infrared emission as concentration increases or quantification of CO2 saturation level in the energy absorption and emission band.

  • @AirwithAri
    @AirwithAri Рік тому

    You are amazing!

  • @brucenassar9077
    @brucenassar9077 Рік тому

    wonderful greta will tell people what to think.

  • @emmanuelibekwe5406
    @emmanuelibekwe5406 Рік тому

    Thank you, Prof.

  • @JamesVestal-dz5qm
    @JamesVestal-dz5qm Рік тому

    Taco bell vorticity energy! Taco bell employees for vestal!

  • @JamesVestal-dz5qm
    @JamesVestal-dz5qm Рік тому

    After my nap I'm researching vorticity!

  • @daveandrews9634
    @daveandrews9634 Рік тому

    The hockey stick handle based on dendrological records is not accurate to any degree whatsoever. It shouldn’t even be shown as resembling anything factual related to global temperatures.

  • @daveandrews9634
    @daveandrews9634 Рік тому

    Tree ring records cannot be used to recreate temperature records. Precipitation is the primary cause of tree ring thickness. Temperature has very little influence on tree ring thicknesses. Droughts and temperature are not well correlated.

    • @DrSmooth2000
      @DrSmooth2000 Рік тому

      Globally should be able to correlate with drying but yes not by one tree or even forest.

  • @DertiDerty
    @DertiDerty Рік тому

    The discussion on sea surface height anomaly don't take into account the effect of wind thas can displace water : by geostrophic way, if you put a westely wind over the ocean at mid-latitudes, you will induce an se surface height gradient. No T or S effects here.

  • @DertiDerty
    @DertiDerty Рік тому

    28:00 I've always learned that Ekman induced vertical motions was basically a low-level effect, so the presentation here is a bit weird i think. To understand vertical motions in the free atmosphere, you have to look at something other than Ekman things.

  • @MrBallynally2
    @MrBallynally2 Рік тому

    Modelling is a great tool but only after a level of certainty about the parameters have been reached. In physics some known factors can be easily established by sheer experience and real live data observations. However, in regards to climate only a very limited amount of parameters are certain. Complicated by a dynamic interactive non equilibrium system one could say with absolute certainty that no model or series of models can be relied upon, not even an average even if they all agree. If the underlying premise or assumption is wrong the outcome is as well. So, if you assume the greenhouse gas theory is right in ALL your models All of them will more or less point to the same thing. Since everyone seems to be focused on Co2 maybe it is best to start the models without that and see how they level up to real time measurements. A lot better than they currently do would be my assumption

  • @MrBallynally2
    @MrBallynally2 Рік тому

    Climate sensitivity to CO2? Any statement about this is simply that but not a statement of fact. Ergo, highly speculative and uncertain especially given the amounts of CO2, its saturation and frequency response. And guess what? The more you zoom in the less certain it becomes. Unfortunately the whole climate discussion in terms of political policies hangs on this one element.

  • @MrBallynally2
    @MrBallynally2 Рік тому

    Upwards radiation fr the surface is clearly very small as it will be drowned out by convection and conduction to a lesser extend. Another point is that the influence of greenhouse gasses is ( as standard) overstated. I understand you need to connect both upwards radiation and greenhouse gasses in order to make your calculations work. However, convection usually trumps radiation as does conduction. Furthermore, the oceans play a bigger role than the Earth's surface in regulating energy transfer. Overall, H2O which includes clouds and water vapour completely dwarfs anything Co2 might do both in its frequency spectrum and saturation points in light of greenhouse gasses which is of course a misnomer but anyway. The assumptions about greenhouse gasses are always stated as if they are fact. I see them more as speculation just like the use of the SB law. It assumes the Earth as a blackbox but both the Earth and the atmosphere do not fit into the SB straightjacket as far as i can see. It seems, pun intended, rather...forced.

    • @MrBallynally2
      @MrBallynally2 Рік тому

      With blackbox i of course mean blackbody..

    • @MrBallynally2
      @MrBallynally2 Рік тому

      I do apologize. I didnt watch the video to the end which deals w ...convection.

  • @Forever-do8zs
    @Forever-do8zs Рік тому

    Hello, at 4:15 why pressure surfaces under the warming arent affected ? I would say that the increase of volume of the layer that is warmed would push down on the surfaces below and distord them?

  • @fractalnomics
    @fractalnomics Рік тому

    47:57 No, snow and water are near-perfect blackbody absorbers. They have an emissivity of near 1, similar to the others. I call that a paradox, but is it true. (I also have the solution).

    • @MrBallynally2
      @MrBallynally2 Рік тому

      Near perfect? Blackbody physics require a vacuum which is obviously not the case on Earth. To simply ignore that part of the SB law is rather convenient for yr argument but goes against it fr a scientific viewpoint. I think yr argument has more to do with albedo..

  • @sisaytadesse-kf3xu
    @sisaytadesse-kf3xu Рік тому

    Thanks a lot

  • @kjr2868
    @kjr2868 Рік тому

    Very poor explanation on the role of H2O as a greenhouse gas! In fact understates the role of water vapor in the atmosphere, which as a molecule is 10x stronger at being excited by infra-red than CO2. H2O makes up 3% of the total atmospheric gases (Nitrogen is 75%, Oxygen 20%), CO2 makes up just 0.04%.

    • @DrSmooth2000
      @DrSmooth2000 Рік тому

      Considered irrelevant. Only way to remove water vapor is to freeze it. Which means geoengineering has proceeded along CO2 removal or sunlight diminishment already

  • @CHEIKHOUMOUCTARDOUCOURE
    @CHEIKHOUMOUCTARDOUCOURE Рік тому

    I'm very interested in the video. can i have it in french language?

  • @adriancook9742
    @adriancook9742 Рік тому

    Hello I'm afraid I can't reflect the opinions of the others who commented here. I watched the first lecture which was predictable by it's nature, no surprise there but suddenly in this second lecture we dive into black body radiation which is something of a heavy concept especially if you haven't come across it before. Furthermore, the equations just dumped in front of the students, myself included, seem almost to shock and put people off. There is no real explanation of the black body radiation and the ensuing calculations are almost completely unhelpfu because they aren't shown, a fail in an exam I might add. So we went from being put to sleep in the first lecture and part of this one, to being thrown under the bus in this one. Sorry but it just makes me so angry when people who are supposed to be teaching others do this.

    • @DertiDerty
      @DertiDerty Рік тому

      If you don't mind me saying so, the concepts invoked here are supposed to be familiar to any high-school student following a scientific curriculum. There's no need to demonstrate such simple calculations (I remind you that the course assumes some basic notions). For example, calculating the energy emitted by the sun : - Surface area of a sphere: 4πR² - With a radius of 700,000 km: 4*3.14*700,000,000² = 6.15*10^18 m². Take Stefan's formula with T=5770K, sigma = 5.670400*10^-8 and multiplying by the area gives: (5.670400*10^-8)*(6.15*10^18)*(5770^4) = 3.86*10^26 Watts (rounded off) An exercise I used to do in high school.

  • @nothingkillsthegrimace3543

    Hi Paul, this is a great video that clearly walks through a problem I've been struggling to wrap my head around. I do have a question on your statement that the kinematic method "tends not to be used" because of inaccuracies in measuring the ageostrophic wind. This is confusing to me because I think it's still very much the case that both ECMWF & the WRF model use the kinematic method as the basis for their omega calculations. Do you mean instead that the kinematic method is rarely used for deriving realistic vertical velocity estimates based off observations? It seems to me like it would still be a viable way of calculating vertical velocity on gridded model output fields. Is this a correct interpretation?

    • @introductiontoatmosphericd284
      @introductiontoatmosphericd284 Рік тому

      Yes, it's rarely used for deriving realistic vertical velocity estimates based off of observations. When it comes to the models, horizontal velocities are known to many digits of accuracy, and so losing one digit of accuracy from the kinematic method is justifiable.

    • @nothingkillsthegrimace3543
      @nothingkillsthegrimace3543 Рік тому

      @@introductiontoatmosphericd284 Ok, great! That helps to clear up a lot of my confusion. Thank you very much for your prompt response!

  • @veronikakerman6536
    @veronikakerman6536 Рік тому

    Thanks for the explanation of vorticity and how it relates to curl of a vector field. Now i understand the math behind some terrible python code.