Comment on "Scaling of atmosphere and ocean temperature correlations in observations and climate models"

Physics – Atmospheric and Oceanic Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

1 page with 2 figures

Scientific paper

10.1103/PhysRevLett.92.039801

In a recent letter [K. Fraedrich and R. Blender, Phys. Rev. Lett. 90, 108501 (2003)], Fraedrich and Blender studied the scaling of atmosphere and ocean temperature. They analyzed the fluctuation functions F(s) ~ s^alpha of monthly temperature records (mostly from grid data) by using the detrended fluctuation analysis (DFA2) and claim that the scaling exponent alpha over the inner continents is equal to 0.5, being characteristic of uncorrelated random sequences. Here we show that this statement is (i) not supported by their own analysis and (ii) disagrees with the analysis of the daily observational data from which the grid monthly data have been derived. We conclude that also for the inner continents, the exponent is between 0.6 and 0.7, similar as for the coastline-stations.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Comment on "Scaling of atmosphere and ocean temperature correlations in observations and climate models" does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Comment on "Scaling of atmosphere and ocean temperature correlations in observations and climate models", we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Comment on "Scaling of atmosphere and ocean temperature correlations in observations and climate models" will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-154239

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.