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The [course_title] course explains tools, data, and ideas related to past climate changes as seen in marine, ice core, and continental records. The course discusses the major Paleoceanographic and paleoclimatic events of the past 2 million. You will also be familiarised with the Quantitative tools such as statistics, factor analysis, time series analysis, simple climatology for interpreting paleoceanographic data. Major topics covered in the course are Oxygen isotope palaeoclimatology, Paleo-ecological temperature estimates, Ice core evidence for climate change, cenozoic paleoceanography and others.  

Assessment

This course does not involve any written exams. Students need to answer 5 assignment questions to complete the course, the answers will be in the form of written work in pdf or word. Students can write the answers in their own time. Each answer needs to be 200 words (1 Page). Once the answers are submitted, the tutor will check and assess the work.

Certification

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Course Credit: MIT

Course Curriculum

Major paleoceanographic and paleoclimatic events of the past 2 million years 01:00:00
Oxygen isotope paleoclimatology – Part I 01:00:00
Oxygen isotope paleothermometry – Part II 01:50:00
Paleo-ecological temperature estimates 01:40:00
Fundamentals of factor analysis: satellite image 00:30:00
Sea-level and climate change: coral reefs on stable and emerging islands 01:45:00
Glacial/interglacial ‘oscillations’: why? time-series analysis 02:20:00
Ice core evidence for climate change 01:40:00
Ice core evidence for climate change (cont.) 02:30:00
Deep-ocean paleoceanography and ocean chemistry 02:25:00
The 14C story 01:55:00
Atmospheric CO2, ocean chemistry, and mechanisms of climate change 02:00:00
Continental evidence for glacial climate change 01:50:00
Lifestyles of the small and calcareous 00:35:00
Coral evidence for temperature, salinity, and nutrient changes 00:25:00
Introduction to cenozoic palenoceanography 00:15:00
Newer tracers 00:15:00
Assessment
Submit Your Assignment 00:00:00
Certification 00:00:00

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