Канал: Adrian Lee

HSI1000: Using the single-layer model Excel visualisation

HSI1000: Using the single-layer model Excel visualisation

Gong Xi Fa Cai 2022

Gong Xi Fa Cai 2022

HSI1000 Week 5 Part IX: Modelling the Atmosphere

HSI1000 Week 5 Part IX: Modelling the Atmosphere

HSI1000 Week 5 Part VIII: Building a Model

HSI1000 Week 5 Part VIII: Building a Model

HSI1000 Week 5 Part VII: On Metaphors

HSI1000 Week 5 Part VII: On Metaphors

HSI1000 Week 5 Part VI: Calculating the Greenhouse Effect

HSI1000 Week 5 Part VI: Calculating the Greenhouse Effect

HSI1000 Week 8 Part VIII: The Danger of Certainty

HSI1000 Week 8 Part VIII: The Danger of Certainty

HSI1000 Week 8 Part VII: Climate Change Mitigation

HSI1000 Week 8 Part VII: Climate Change Mitigation

HSI1000 Week 8 Part VI: Principles to Govern International Action

HSI1000 Week 8 Part VI: Principles to Govern International Action

HSI1000 Week 8 Part V: Projections of Climate Change

HSI1000 Week 8 Part V: Projections of Climate Change

HSI1000 Week 8 Part IV: Narratives of the Future

HSI1000 Week 8 Part IV: Narratives of the Future

HSI1000 Week 8 Part III: Models of the Past

HSI1000 Week 8 Part III: Models of the Past

HSI1000 Week 8 Part II: Feedback

HSI1000 Week 8 Part II: Feedback

HSI1000 Week 8 Part I: Reliability of Models

HSI1000 Week 8 Part I: Reliability of Models

HSI1000 Week 7 Part VIII: Cognitive Bias

HSI1000 Week 7 Part VIII: Cognitive Bias

HSI1000 Week 7 Part VII: Climate Change Myths:“It’s not us”

HSI1000 Week 7 Part VII: Climate Change Myths:“It’s not us”

HSI1000 Week 7 Part VI: Climate Change Myths:“Animals and plants can adapt”

HSI1000 Week 7 Part VI: Climate Change Myths:“Animals and plants can adapt”

HSI1000 Week 7 Part V: Climate Change Myths:“The Earth’s cooling”

HSI1000 Week 7 Part V: Climate Change Myths:“The Earth’s cooling”

HSI1000 Week 7 Part IV: Climate Change Myths:“It’s the sun”

HSI1000 Week 7 Part IV: Climate Change Myths:“It’s the sun”

HSI1000 Week 7 Part III: Climate Change Myths:“Climate’s changed before”

HSI1000 Week 7 Part III: Climate Change Myths:“Climate’s changed before”

HSI1000 Week 7 Part II: When Scientists Know Sin

HSI1000 Week 7 Part II: When Scientists Know Sin

HSI1000 Week 7 Part I: The Art of Doubt

HSI1000 Week 7 Part I: The Art of Doubt

HSI1000 Week 6 Part VIII: On the Nature of Scientific Understanding

HSI1000 Week 6 Part VIII: On the Nature of Scientific Understanding

HSI1000 Week 6 Part VII: Anthropogenic or Natural

HSI1000 Week 6 Part VII: Anthropogenic or Natural

HSI1000 Week 6 Part VI: Concomitant Rise in Greenhouse Gases

HSI1000 Week 6 Part VI: Concomitant Rise in Greenhouse Gases

HSI1000 Week 6 Part V: Unprecedented

HSI1000 Week 6 Part V: Unprecedented

HSI1000 Week 6 Part IV: Temperature Rising

HSI1000 Week 6 Part IV: Temperature Rising

HSI1000 Week 6 Part III: Not a Question of If, a Question of When

HSI1000 Week 6 Part III: Not a Question of If, a Question of When

HSI1000 Week 6 Part II: History of a Developing Consensus

HSI1000 Week 6 Part II: History of a Developing Consensus

HSI1000 Week 5 Part IV: Problem of Combustion

HSI1000 Week 5 Part IV: Problem of Combustion

HSI1000 Week 6 Part I: Climate Change and the Scientific Consensus

HSI1000 Week 6 Part I: Climate Change and the Scientific Consensus

HSI1000 Week 5 Part V: Role of the Atmosphere

HSI1000 Week 5 Part V: Role of the Atmosphere

HSI1000 Week 5 Part III: Nature of the Atmosphere

HSI1000 Week 5 Part III: Nature of the Atmosphere

HSI1000 Week 5 Part II: Discovery of the Greenhouse Effect

HSI1000 Week 5 Part II: Discovery of the Greenhouse Effect

HSI1000 Week 5 Part I: Epistemic Responsibility

HSI1000 Week 5 Part I: Epistemic Responsibility

Using Solver to determine temperature

Using Solver to determine temperature

transforming practice

transforming practice

using solver to do least squares minimisation

using solver to do least squares minimisation

Using LINEST

Using LINEST

Using Excel to calculate the ozone profile

Newton-Raphson method using Excel

Newton-Raphson method using Excel

Vibrational Spectroscopy - Part XI

Vibrational Spectroscopy - Part XI

Vibrational Spectroscopy - Part X

Vibrational Spectroscopy - Part X

Vibrational Spectroscopy - Part IX

Vibrational Spectroscopy - Part IX

Vibrational Spectroscopy - Part VIII

Vibrational Spectroscopy - Part VIII

Using Solver

Using Solver

Using StatPlus

Using StatPlus

Data Regression using Excel

Data Regression using Excel

Vibrational Spectroscopy - Part VII

Vibrational Spectroscopy - Part VII

Vibrational Spectroscopy - Part VI

Vibrational Spectroscopy - Part VI

Vibrational Spectroscopy - Part V

Vibrational Spectroscopy - Part V

Vibrational Spectroscopy - Part IV

Vibrational Spectroscopy - Part IV

Vibrational Spectroscopy - Part III

Vibrational Spectroscopy - Part III

Vibrational Spectroscopy - Part II

Vibrational Spectroscopy - Part II

Vibrational Spectroscopy - Part I

Vibrational Spectroscopy - Part I

ESO Taurus Molecular Cloud

ESO Taurus Molecular Cloud

Rotational Spectroscopy - Part XII

Rotational Spectroscopy - Part XII

Rotational Spectroscopy - Part XI

Rotational Spectroscopy - Part XI

Rotational Spectroscopy - Part X

Rotational Spectroscopy - Part X

Rotational Spectroscopy - Part XIII

Rotational Spectroscopy - Part XIII

Rotational Spectroscopy - Part IX

Rotational Spectroscopy - Part IX

Rotational Spectroscopy - Part VIII

Rotational Spectroscopy - Part VIII

Rotational Spectroscopy - Part VII

Rotational Spectroscopy - Part VII

Rotational Spectroscopy - Part VI

Rotational Spectroscopy - Part VI

Rotational Spectroscopy - Part V

Rotational Spectroscopy - Part V

Rotational Spectroscopy - Part IV

Rotational Spectroscopy - Part IV

Rotational Spectroscopy - Part III

Rotational Spectroscopy - Part III

Rotational Spectroscopy - Part II

Rotational Spectroscopy - Part II

Rotational Spectroscopy - Part I

Rotational Spectroscopy - Part I