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| '''Lars Kaleschke, Alexander Loew''' | |
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| MS Integrated Climate System Sciences Date: 3.2.2014-7.2.2014 Place: Geom 1536c |
'''Lars Kaleschke, Alexander Loew''' MS Integrated Climate System Sciences; Date: 3.2.2014-7.2.2014; Place: Geom 1536c |
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| Morning: Group presentations of project plan and preliminary analysis. Afternoon: implementation and project work |
Morning: Group presentations of project plan and preliminary analysis; Afternoon: implementation and project work |
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| Morning: Group presentations of methods and code implementations Afternoon: Project work |
Morning: Group presentations of methods and code implementations; Afternoon: Project work |
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| Morning: Group presentations of preliminary results Afternoon: Project work |
Morning: Project work, preparation of presentation; '''14:00-16:00 final presentation (B, A, C)''' of results and discussion, evaluation |
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| Morning: final presenation of results and discussion Afternoon: evaluation and preparation of final report |
Morning: project work, preparation of final report |
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| Kevin Cowtan and Robert Way published [[http://onlinelibrary.wiley.com/doi/10.1002/qj.2297/abstract | a paper]] which was quite controverily discussed in the scientific community. They fill gaps of the HadCRUT temperature data set by using satellite data. By filleing this (well known) Arctic gap and compare their new reconstruction of surface temperature data to independent in-situ observations and reanalysis data they show that the global mean temperature hiatus is not observable any more. | Kevin Cowtan and Robert Way published [[http://onlinelibrary.wiley.com/doi/10.1002/qj.2297/abstract | a paper]] which was quite controverily discussed in the scientific community. They fill gaps of the HadCRUT temperature data set by using satellite data. By filling this (well known) Arctic gap and compare their new reconstruction of surface temperature data to independent in-situ observations and reanalysis data they show that the global mean temperature hiatus is not observable any more. |
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Some further reading ... * [[http://www.nature.com/ngeo/journal/v7/n2/full/ngeo2078.html | Uncertain temperature trend]] * [[http://www.scilogs.de/klimalounge/erwaermung-unterschaetzt/?utm_source=rss&utm_medium=rss&utm_campaign=erwaermung-unterschaetzt | Erderwaermung unterschaetzt]] |
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| * how robust are trends estimated from this data record? What is the role of the length of the timeperiod? * do the same analysis for the original HadCRU temperature dataset (and possibly also for other datasets, like reanalysis (cross-check with Project C !)) |
* how robust are trends estimated from this data record? What is the role of the length and starting point of the timeperiod? * [do the same analysis for the original HadCRU temperature dataset (and possibly also for other datasets, like reanalysis (cross-check with Project C !))]; this is optional and of lower priority |
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| === Project B: Variations in Surface Air Temperature Observations in the Arctic === | === Project B: Spatial Correlations of Surface Air Temperature Observations in the Arctic === Main research question: over what distances are surface temperatures correlated? |
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| * Analyse the surface air temperature measured by the drift buoys (seasonal cycle, anomalies, trends etc.) * Are there significant trends over different period of times? |
* Analyse the surface air temperature (monthly mean gridded products) measured by the drift buoys * Calculate seasonal cycle, anomalies, and linear trends * Estimate the (radial) spatial (auto)correlation of surface temperature anomalies * Present all results in proper form (timeseries, maps, statistics ...) |
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| * [[http://iabp.apl.washington.edu/AirT/RigorEtal-SAT.pdf|Rigor, I., R. Colony, and S. Martin, 2000, Variations in Surface Air Temperature Observations in the Arctic, 1979 - 1997, J. Climate, Vol. 13, no 5, 896-914.]] | [[http://iabp.apl.washington.edu/AirT/RigorEtal-SAT.pdf|Rigor, I., R. Colony, and S. Martin, 2000, Variations in Surface Air Temperature Observations in the Arctic, 1979 - 1997, J. Climate, Vol. 13, no 5, 896-914.]] |
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| === Project C: Data intercomparison === | === Project C: Data Intercomparison === |
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| Use the buoy measurements of surface air temperature as ground truth | Comparison and validation - how do we know the ground truth? |
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| * Write code to interpolate the different datasets in a common grid * Compare CW2013, buoy and reanalysis data |
* Compare HADCRUT4, HADCRUT4 hybrid (CW2013), IABP Arctic surface air temperature measurements, and reanalysis data |
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| * Are there biases or jumps in the data? | * Are there relative biases or jumps in the data? * What is the air temperature over a melting sea ice surface during Summer? * Can you judge which data are most reliable? Discuss! * Present all results in proper form (timeseries, maps, statistics ...) Lüpkes, C., Vihma, T., Jakobson, E., König-Langlo, G., and Tetzlaff, A.: Meteorological observations from ship cruises during summer to the Central Arctic: A comparison with reanalysis data, Geophys. Res. Lett., 27, L09810, doi:10.1029/2010GL042724, 2010. |
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| * [[http://www.hoaps.org|HOAPS climatology]] of ocean surface fluxes * HOAPS is sampled twice a day * What is the impact of undersampling the dirnal cycle on monthly means? * What is the impact of sea ice gaps on monthly means? * How do HOAPS surface flux estimates compare to literature values of global mean ocean surface fluxes? * What is the impact of different land/sea masks and spatial grids (resolution, projections) on total mean global fluxes? |
The Meteorological Institute of the University of Hamburg and the Max-Planck-Institute for Meteorology have compiled a climate data record of ocean surface fluxes. This so called [[http://www.hoaps.org|HOAPS climatology]] has been sucessfully applied in numerous studies and is one of a very few global records on ocean surface fluxes. HOAPS is uniquely built based on satellite data. Major references for HOAPS can be found on the [[http://www.hoaps.org | project website]]. Details of the algorithms and data processing are provided in [[http://www.earth-syst-sci-data.net/2/215/2010/ | Andersson et al. (2010)]] and [[http://journals.ametsoc.org/doi/abs/10.1175/2010JAMC2341.1 | Andersson et al (2011)]]. The HOAPS dataset is based on sampling twice a day, which is due to the overpass time of the satellites used to generate the product. The project shall address the following research questions: * What is the impact of undersampling the diurnal cycle? * are biases introduced in e.g. monthly means? * what is the impact of sea ice gaps on monthly means? * What is the effec of different land/sea masks and spatial grids (resolution, projections) on total mean global fluxes? * do total mean global numbers change? If so, by how much? * how do global mean flux estimats from HOAPS compare to other datasets available? * How are HOAPS surface fluxes related to climate indices like e.g. NAO, PDO, ENSO ... ? * as a starting point the paper from [[http://tellusa.net/index.php/tellusa/article/view/15710 | Andersson et al (2010) ]] might be usefull * develop appropriate metrices (e.g. different correlation approaches, EOF) for comparing HOAPS surface fluxes with climate indices |
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| = TODOs = == Data == * CW2013 :-) * ERA-Interim :-) * NCEP :-) * Bouy data :-) * HOAPS data :-) |
= Extra support = |
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| == Final report == | [[/IABP_Buoy_Data]] = Final report = == Group Report == |
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| * Conlcusion | * Conclusion * Disclaimer (individual contributions) |
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| == References == * [[https://wiki.zmaw.de/ifm/FrontPage/Python|Python at KlimaCampus]] * Python Scripting for Computational Science, Hans Petter Langtangen, Springer (available in the ZMAW library) |
Please indicate the responsible authors for the different sections within the report! == Individual Reports == (1 page) * What have you learned during the course? * What was your individual contribution to the project and to the group report? |
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= Python References = * [[https://wiki.zmaw.de/ifm/FrontPage/Python|Python at KlimaCampus]] * Python Scripting for Computational Science, Hans Petter Langtangen, Springer (available in the ZMAW library) |
Contents
63-953 Climate and Satellite Data Analysis
Lars Kaleschke, Alexander Loew MS Integrated Climate System Sciences; Date: 3.2.2014-7.2.2014; Place: Geom 1536c
Course objectives
The participants will learn to practically work with climate model, reanalysis, in-situ station and satellite data. Organized as a group project, the participants will further learn the principles of project management and shared software development.
Schedule
Monday, 10:00
General Introduction
Group work: develop a project plan and write a short technical proposal for your project.
Final report due by 15. March 2014
Obtain data and do preliminary analysis (e.g. data coverage).
Tuesday
Morning: Group presentations of project plan and preliminary analysis; Afternoon: implementation and project work
Wednesday
Morning: Group presentations of methods and code implementations; Afternoon: Project work
Thursday
Morning: Project work, preparation of presentation; 14:00-16:00 final presentation (B, A, C) of results and discussion, evaluation
Friday
Morning: project work, preparation of final report
Topics for group work
The major topic of this course will deal with data gaps in climate and satellite records and their implications for the calculation of global statistics. The overall objectives of the course are:
- raise awareness on the problem with data gaps in climate records
- learn about methods for coping with data gaps
- assess the effect of data gaps on statistics of climate related datasets
- learn processing of data using a variety of methods
Another major objective of this course is to train the so called soft-skills in practice, like
- project management (planning ... final report)
- joint code development
- reporting
Has the Earth stopped warming?
Coverage bias in the HadCRUT4 temperature series and its impact on recent temperature trends
Kevin Cowtan and Robert Way published a paper which was quite controverily discussed in the scientific community. They fill gaps of the HadCRUT temperature data set by using satellite data. By filling this (well known) Arctic gap and compare their new reconstruction of surface temperature data to independent in-situ observations and reanalysis data they show that the global mean temperature hiatus is not observable any more.
Cowtan and Way (2013) methods and data are freely available and we will use them in the course:
Some further reading ...
In situ measurements of surface temperatures are available from the International Arctic Buoy Programme (IABP) website:
Project A: Cowtan and Way (CW2013) reconstruction
- Review methods of Cowtan and Way (2013) and give a summary of their approach
- Analyse their reconstructed dataset of surface air temperature in terms of different parameters (global mean and stdv, seasonal cycle, anomalies, trends etc.)
- is the dataset homogeneous in time or can you observe temporal inconsistencies?
- how robust are trends estimated from this data record? What is the role of the length and starting point of the timeperiod?
- [do the same analysis for the original HadCRU temperature dataset (and possibly also for other datasets, like reanalysis (cross-check with Project C !))]; this is optional and of lower priority
- are results different? are they significantly different?
- Look at correlations with climate indices, e.g. ENSO, NAO, PDO
- Present all results in proper form (maps, statistics ...)
Project B: Spatial Correlations of Surface Air Temperature Observations in the Arctic
Main research question: over what distances are surface temperatures correlated?
- Review methods of Rigor et al. (2000)
- Analyse the surface air temperature (monthly mean gridded products) measured by the drift buoys
- Calculate seasonal cycle, anomalies, and linear trends
- Estimate the (radial) spatial (auto)correlation of surface temperature anomalies
- Present all results in proper form (timeseries, maps, statistics ...)
Project C: Data Intercomparison
Comparison and validation - how do we know the ground truth?
- Compare HADCRUT4, HADCRUT4 hybrid (CW2013), IABP Arctic surface air temperature measurements, and reanalysis data
- Was the data gap in the Arctic filled in reasonably?
- Are there relative biases or jumps in the data?
- What is the air temperature over a melting sea ice surface during Summer?
- Can you judge which data are most reliable? Discuss!
- Present all results in proper form (timeseries, maps, statistics ...)
Lüpkes, C., Vihma, T., Jakobson, E., König-Langlo, G., and Tetzlaff, A.: Meteorological observations from ship cruises during summer to the Central Arctic: A comparison with reanalysis data, Geophys. Res. Lett., 27, L09810, doi:10.1029/2010GL042724, 2010.
Project D: HOAPS ocean flux sampling bias
The Meteorological Institute of the University of Hamburg and the Max-Planck-Institute for Meteorology have compiled a climate data record of ocean surface fluxes. This so called HOAPS climatology has been sucessfully applied in numerous studies and is one of a very few global records on ocean surface fluxes. HOAPS is uniquely built based on satellite data.
Major references for HOAPS can be found on the project website. Details of the algorithms and data processing are provided in Andersson et al. (2010) and Andersson et al (2011).
The HOAPS dataset is based on sampling twice a day, which is due to the overpass time of the satellites used to generate the product.
The project shall address the following research questions:
* What is the impact of undersampling the diurnal cycle?
- are biases introduced in e.g. monthly means?
- what is the impact of sea ice gaps on monthly means?
* What is the effec of different land/sea masks and spatial grids (resolution, projections) on total mean global fluxes?
- do total mean global numbers change? If so, by how much?
- how do global mean flux estimats from HOAPS compare to other datasets available?
* How are HOAPS surface fluxes related to climate indices like e.g. NAO, PDO, ENSO ... ?
as a starting point the paper from Andersson et al (2010) might be usefull
- develop appropriate metrices (e.g. different correlation approaches, EOF) for comparing HOAPS surface fluxes with climate indices
Extra support
Final report
Group Report
Template structure:
- Abstract
- Introduction: state of the art (literature), statement of the problem
- Methods and data
- Results
- Discussion
- Conclusion
- Disclaimer (individual contributions)
Please indicate the responsible authors for the different sections within the report!
Individual Reports
(1 page)
- What have you learned during the course?
- What was your individual contribution to the project and to the group report?
Examples from the past
How significant are observations of Arctic temperature trends?
Python References
- Python Scripting for Computational Science, Hans Petter Langtangen, Springer (available in the ZMAW library)