Section 13.1 – A Closer Look at Earth
... Section 14.1 and 14.2 - North American Weather Systems 1. Know what a meteorologist is. 2. Recognize Bernoulli’s principle and that as wind speeds up it becomes less dense. 3. Know what weather systems are and which direction they tend to move in North America 4. Know what Air masses are and be able ...
... Section 14.1 and 14.2 - North American Weather Systems 1. Know what a meteorologist is. 2. Recognize Bernoulli’s principle and that as wind speeds up it becomes less dense. 3. Know what weather systems are and which direction they tend to move in North America 4. Know what Air masses are and be able ...
regional climate model intercomparison project for asia
... MRI model, which are 1°–3°C too warm over Japan temperature, the three areas of the China mainland, and Korea. Japanese islands, and Korean peninsula are chosen for It is also worth noting that Fig. 2 presents signifi- a quantitative assessment of precipitation bias, which cant diversity among the m ...
... MRI model, which are 1°–3°C too warm over Japan temperature, the three areas of the China mainland, and Korea. Japanese islands, and Korean peninsula are chosen for It is also worth noting that Fig. 2 presents signifi- a quantitative assessment of precipitation bias, which cant diversity among the m ...
01_COPES_in_Poznan
... Systematic re-processing and coordinated reanalysis of all available observations acquired from various satellite sensors and other data sources since several decades • Would be complementary to model re-analyses in order to define “present climate” • Would serve as a benchmark to validate climate m ...
... Systematic re-processing and coordinated reanalysis of all available observations acquired from various satellite sensors and other data sources since several decades • Would be complementary to model re-analyses in order to define “present climate” • Would serve as a benchmark to validate climate m ...
Carbon-nitrogen cycle coupling regulates climate
... Land components of climate-carbon cycle feedback ...
... Land components of climate-carbon cycle feedback ...
Climate Change Risk and Uncertainty Exercise 1: Temperature
... In the rst part of the exercise, we will create a toy model based on the observed time series. After that, we will compare the observations and our toy model with results from two global climate models (CESM and MPI-ESM). In the end, we will calculate impact costs associated with future temperature ...
... In the rst part of the exercise, we will create a toy model based on the observed time series. After that, we will compare the observations and our toy model with results from two global climate models (CESM and MPI-ESM). In the end, we will calculate impact costs associated with future temperature ...
Slide 1
... model-observational comparisons • Synthesis papers published documenting SE Pacific clouds and atmospheric structure, composition and variability sampled along 20oS during VOCALS-REx, Allen et al. (2011) and Bretherton et al. (2010) • Seven years of VOCALS cruise data compiled along 20oS and describ ...
... model-observational comparisons • Synthesis papers published documenting SE Pacific clouds and atmospheric structure, composition and variability sampled along 20oS during VOCALS-REx, Allen et al. (2011) and Bretherton et al. (2010) • Seven years of VOCALS cruise data compiled along 20oS and describ ...
Project summary (in German and English, max
... is controlled by individually contributing factors taking effect in differing time scales (episodically, seasonally, in the long term). SeRAC-CC aims at evaluating the influence of changes of temperature and precipitation conditions on the system state and thus on the resulting runoff reaction of sm ...
... is controlled by individually contributing factors taking effect in differing time scales (episodically, seasonally, in the long term). SeRAC-CC aims at evaluating the influence of changes of temperature and precipitation conditions on the system state and thus on the resulting runoff reaction of sm ...
PPT
... Methane is “win-win” – but only as part of a global strategy Effect on surface ozone air quality is through decrease in ozone background and does not depend on where methane emission is reduced ...
... Methane is “win-win” – but only as part of a global strategy Effect on surface ozone air quality is through decrease in ozone background and does not depend on where methane emission is reduced ...
The BBVA Foundation honors the authors of the mathematical
... Oceanic Sciences at Princeton University (United States), stresses the importance of his colleague’s contribution: “I started working with models earlier, but Hansen was the first to use these models to make predictions.” This effort, and his own, have underpinned the pathway to the present juncture ...
... Oceanic Sciences at Princeton University (United States), stresses the importance of his colleague’s contribution: “I started working with models earlier, but Hansen was the first to use these models to make predictions.” This effort, and his own, have underpinned the pathway to the present juncture ...
514 kb
... Oceanic Sciences at Princeton University (United States), stresses the importance of his colleague’s contribution: “I started working with models earlier, but Hansen was the first to use these models to make predictions.” This effort, and his own, have underpinned the pathway to the present juncture ...
... Oceanic Sciences at Princeton University (United States), stresses the importance of his colleague’s contribution: “I started working with models earlier, but Hansen was the first to use these models to make predictions.” This effort, and his own, have underpinned the pathway to the present juncture ...
Lecture 6
... Ebers–Moll Model • The classic mathematical model for the bipolar junction transistor is the Ebers-Moll model formulated by J. J. Ebers and J. L. Moll from Bell Laboratories in the early 1954. • Ebers-Moll model also known as “Coupled Diode Model” • The Ebers-Moll model provides an alternative view ...
... Ebers–Moll Model • The classic mathematical model for the bipolar junction transistor is the Ebers-Moll model formulated by J. J. Ebers and J. L. Moll from Bell Laboratories in the early 1954. • Ebers-Moll model also known as “Coupled Diode Model” • The Ebers-Moll model provides an alternative view ...
ENSEMBLES Project Plan WP 6
... and RT2B RCM simulations: first at spatial scales of 50 km at a European-wide scale and later also at as high a resolution as 20 km for specified sub-regions (diffenrent scales but same forcing) RT2B: Production of regional climate scenarios for impact assessments o Same model versions as RT3 o 1950 ...
... and RT2B RCM simulations: first at spatial scales of 50 km at a European-wide scale and later also at as high a resolution as 20 km for specified sub-regions (diffenrent scales but same forcing) RT2B: Production of regional climate scenarios for impact assessments o Same model versions as RT3 o 1950 ...
Weather PPT - Killeen ISD
... tornados. They are the tallest of all clouds and have an anvil shaped top due to the stronger winds at those altitudes. ...
... tornados. They are the tallest of all clouds and have an anvil shaped top due to the stronger winds at those altitudes. ...
The "Greenhouse Effect" as a Function of Atmospheric Mass
... simplify calculations, some restrictions in planetary atmospheric conditions are introduced in a thought experiment involving an idealised planetary body. This technique isolates the atmospheric mass influence and then determines the value of GE when both the influence of radiative interaction with ...
... simplify calculations, some restrictions in planetary atmospheric conditions are introduced in a thought experiment involving an idealised planetary body. This technique isolates the atmospheric mass influence and then determines the value of GE when both the influence of radiative interaction with ...
Atmospheric Science
... tropical depression and storm, diurnal variation of surface pressure, surface and air temperature, wind, rainfall, humidity and cloudiness, basic ideas of general circulation (without mathematical derivations). Synoptic Introduction to synoptic meteorology, scales of weather systems, synoptic weathe ...
... tropical depression and storm, diurnal variation of surface pressure, surface and air temperature, wind, rainfall, humidity and cloudiness, basic ideas of general circulation (without mathematical derivations). Synoptic Introduction to synoptic meteorology, scales of weather systems, synoptic weathe ...
PPT - cmmap
... Treut and McAvaney, 2000). The models are coupled to a slab ocean mixed layer and are brought to equilibrium for present climatic conditions and for a double CO2 climate. The sign is positive when an increase of the CRF (from present to double CO2 conditions) increases the warming, negative when it ...
... Treut and McAvaney, 2000). The models are coupled to a slab ocean mixed layer and are brought to equilibrium for present climatic conditions and for a double CO2 climate. The sign is positive when an increase of the CRF (from present to double CO2 conditions) increases the warming, negative when it ...
Name: Date: Period: ______ Unit 4 – Meteorology Review (CH 22
... 18. How does radiation travel and at what speed does it travel? 19. What molecules are in the thermosphere and mesosphere and what do they absorb? 20. What affect does U.V. rays have in the stratosphere? 21. What absorbs infrared radiation in the troposphere? 22. What happens to solar energy that re ...
... 18. How does radiation travel and at what speed does it travel? 19. What molecules are in the thermosphere and mesosphere and what do they absorb? 20. What affect does U.V. rays have in the stratosphere? 21. What absorbs infrared radiation in the troposphere? 22. What happens to solar energy that re ...
Document
... Projected surface temperature changes for the early and late 21st century relative to the period 1980– 1999 ...
... Projected surface temperature changes for the early and late 21st century relative to the period 1980– 1999 ...
Atmospheric model
An atmospheric model is a mathematical model constructed around the full set of primitive dynamical equations which govern atmospheric motions. It can supplement these equations with parameterizations for turbulent diffusion, radiation, moist processes (clouds and precipitation), heat exchange, soil, vegetation, surface water, the kinematic effects of terrain, and convection. Most atmospheric models are numerical, i.e. they discretize equations of motion. They can predict microscale phenomena such as tornadoes and boundary layer eddies, sub-microscale turbulent flow over buildings, as well as synoptic and global flows. The horizontal domain of a model is either global, covering the entire Earth, or regional (limited-area), covering only part of the Earth. The different types of models run are thermotropic, barotropic, hydrostatic, and nonhydrostatic. Some of the model types make assumptions about the atmosphere which lengthens the time steps used and increases computational speed.Forecasts are computed using mathematical equations for the physics and dynamics of the atmosphere. These equations are nonlinear and are impossible to solve exactly. Therefore, numerical methods obtain approximate solutions. Different models use different solution methods. Global models often use spectral methods for the horizontal dimensions and finite-difference methods for the vertical dimension, while regional models usually use finite-difference methods in all three dimensions. For specific locations, model output statistics use climate information, output from numerical weather prediction, and current surface weather observations to develop statistical relationships which account for model bias and resolution issues.