Husam El Alqamy, B.Sc, M.Phil.
Sr. Biodiversity GIS Analyst,
Enivronmental Information Sector
Environment Agency - Abu Dhabi
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http://dx.doi.org/10.1002/joc.1322
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Hi,
Ahmed, I think the question should perhaps not be what is the maximum uncertainty that should be avoided in the [distribution] data, but rather what is the likely impact of quality variation in the distribution data on model output given the other sources of uncertainty present in the model. There are obviously trade-offs involved. I also wonder if using land use as a covariate for projecting into the future is useful. Do you have a way for factoring in future representations for land use (it doesn’t strike me as an obvious choice for a static variable)?
As Husam points out, there are sources of data other that WorldClim that may be better to use for your modelling. At a global level, the CliMond dataset has improved on some of the limitations with the WorldClim data and at a regional level there may be other datasets available with additional variables that are more ecologically relevant to your modelled species and the scale of the model you are constructing.
The problem with the term relative (as in “relatively high uncertainty”) is that, well, it’s relative! This reinforces my initial point that everyone will need to consider their own particular situation and the unique context it will inevitably have. There is certainly no one resolution rule to fit all. I see that Bruce Miller makes a similar point on this thread: http://groups.google.com/group/maxent/browse_thread/thread/0c8918c3b0075ac8#
As, for example, Elith & Leathwick (2009; http://dx.doi.org/10.1146/annurev.ecolsys.110308.120159) point out, choice of resolution depends on issues such as the spatial accuracy of the data, characteristics of the terrain, life history and putative range determining factors for the species, and the intended application of the modelling exercise.
Do keep in mind that (i) many of the GCM anomaly surfaces are almost 2° resolution in their native form, (ii) in many parts of the world the station data underpinning the global gridded datasets are hundreds of kilometres apart (e.g. Fig 1 in http://dx.doi.org/10.1002/joc.1276), and (iii) that topographic heterogeneity can lead to steep covariate gradients over short geographical distances.
I’ll say again that when modelling over large areas, what appears to be a default choice in many papers of using the finest available gridded data without careful consideration seems a surprising one. Perhaps the one exception I can think of where dropping down to finer scales makes sense is where high topographic variation may be influencing the projection suitability at its range margins (i.e. a finer resolution would allow the user to pick up on this variability).
Either way, I would recommend reading the section entitled “Spatial Scale” in Elith & Leathwick (2009) and some of the references in their Supplemental Literature as a starting point for a better understanding of these issues.
I hope that helps a little bit and good luck!