Go to homepage
Find educational resourcesKnowledge & expertiseCommunities
NL|EN
Privacy policyParticipating institutions
Creative CommonsCreative Commons AttributionSURFFunded by the European Union
Publisher:Meteorology and Air Quality Group, Wageningen University

Filter

Search results (12)

HBO/WO

MBO

July 7, 2020

Rubric for assessment of MSc-thesis

Assessment rubric for master thesis at Wageningen University, in use since 2010. Version: 1.1. The rubric has been developed to match the criteria used in the compulsory assessment form used throughout the University. The rubric is intended to clarify expectations to students, enable conversations about grading en homogenize assessment between assessors.

Document

Arnold Moene, Blair van Pelt

2017

Clip7c Atmospheric Dynamics -Thermal wind

In this clip I will show an application of the theory of geostrategic motion using the case of a change in the geostrategic wind with height. You will see that this change is closely linked to an existing horizontal temperature gradient. We start with two columns of air. The left column is filled with cold air. And the right column with more Mer. The clip relates to the course Introduction Atmosphere (MAQ-10306; https://ssc.wur.nl/Handbook/Course/MAQ-10306).

Video

Arnold Moene

2017

Clip7b Atmospheric Dynamics

In this clip I will illustrate the theory of juice trophic motion by using the example of curved isobars We will also examine the theory of circular motion and learn how to derive the gradient wind relationships. The clip relates to the course Introduction Atmosphere (MAQ-10306; https://ssc.wur.nl/Handbook/Course/MAQ-10306).

Video

Arnold Moene

2017

Clip1b: Introduction to the Atmosphere

In this clip I will give you a brief overview of one of the fundamental laws concerning the atmosphere the ideal gas law for any gas or mixture of gases the pressure within a given volume is determined by the temperature and the number of molecules in that volume. The clip relates to the course Introduction Atmosphere (MAQ-10306; https://ssc.wur.nl/Handbook/Course/MAQ-10306).

Video

Arnold Moene

2017

Clip7a: Atmopsheric Dynamics

The atmosphere is in constant motion. Motions are caused by and subject to a number of different forces. In this clip we will examine the fundamental forces involved in atmospheric motion. The clip relates to the course Introduction Atmosphere (MAQ-10306; https://ssc.wur.nl/Handbook/Course/MAQ-10306).

Video

Arnold Moene

2017

Clip3: Thermodynamic diagrams

Performing calculations of thermodynamic processes in the atmosphere is often cumbersome Furthermore graphical representation of the vertical profiles for temperature and humidity as measured by radiosonde require consistency. For both applications thermodynamic diagrams are a very powerful solution in this clip I will explain how these diagrams are constructed and present a few elementary applications. (MAQ-10306; https://ssc.wur.nl/Handbook/Course/MAQ-10306).

Video

Arnold Moene

2017

Clip4a: Radiation

Radiation from the sun is the sole reason that Earth can sustain life. It is also the driving force behind many of the movements that we see happening in the atmosphere and the oceans. In this clip we will examine fundamental radiation laws and take a close look at solar radiation. The clip relates to the course Introduction Atmosphere (MAQ-10306; https://ssc.wur.nl/Handbook/Course/MAQ-10306).

Video

Arnold Moene

2017

Clip2b: Atmospheric Humidity

Well water in its many phases plays a crucial role in the atmosphere as well as in the climate in this clip I will explain the essential properties of water vapor and the different ways to express the amount of humidity in the air. Let's start by making an important distinction between a gas and a vapor. The clip relates to the course Introduction Atmosphere (MAQ-10306; https://ssc.wur.nl/Handbook/Course/MAQ-10306).

Video

Arnold Moene

2017

Clip10: Atmospheric Turbulence

The flow of air through the atmosphere is not always smooth and steady sometimes the airflow becomes erratic and unsteady the flow is then said to be turbulent. A good example of this turbulence occurs in the layer of air close to the ground. Strong turbulence during the daytime can cause this layer of air to grow to a height of one to two kilometers with small clouds forming on the top. In this clip we will take a closer look at turbulence its origin and description I will also discuss the vertical fluxes that it generates turbulence can also be found on a much smaller scale take these two examples here. The clip relates to the course Introduction Atmosphere (MAQ-10306; https://ssc.wur.nl/Handbook/Course/MAQ-10306).

Video

Arnold Moene

2017

Clip2a: Thermodynamics

In this clip I will present an overview of two fundamental concepts in meteorology hydrostatic equilibrium and the First Law of Thermodynamics. The clip relates to the course Introduction Atmosphere (MAQ-10306; https://ssc.wur.nl/Handbook/Course/MAQ-10306).

Video

Arnold Moene