This study evaluates the performance of two bias correction techniques—power transformation and gamma distribution adjustment—for Eta regional climate model (RCM) precipitation simulations. For the gamma distribution adjustment, the number of dry days is not taken as a fixed parameter; rather, we propose a new methodology for handling dry days. We consider two cases: the first case is defined as having a greater number of simulated dry days than the observed number, and the second case is defined as the opposite. The present climate period was divided into calibration and validation sets. We evaluate the results of the two bias correction techniques using the Kolmogorov-Smirnov nonparametric test and the sum of the differences between the cumulative distribution curves. These tests show that both correction techniques were effective in reducing errors and consequently improving the reliability of the simulations. However, the gamma distribution correction method proved to be more efficient, particularly in reducing the error in the number of dry days.
The common geostrophic estimation of ocean current velocity uses only water temperature and conductivity profiles. The geostrophic
volume transport of a western boundary current, like the Taiwan Current (Kuroshio east of Taiwan), between the coast and its
eastern boundary can be easily estimated based on hydrographic survey data. But the eastern boundary of the Taiwan Current
is very uncertain due to extremely variable hydrographic conditions. This uncertainty is strongly correlated with the propagating
mesoscale eddies originating from the interior of the western North Pacific Ocean. The uncertainty of estimated transport
can be greatly reduced if eddy distribution is considered when determining the integration boundaries with the assistance
of satellite altimeter measurements. Eight hydrographic surveys east of Taiwan between November 1992 and June 1996 are demonstrated
in this study. The average geostrophic transport of the Taiwan Current with a reference set to 1000 dbar at 22°N between the
east coast of Taiwan and 124°E is 22.9 ±14.2 Sv and changes to 22.1 ± 8.3 Sv, the uncertainty of which is nearly halved after
taking account of the eddy distribution. The estimation uncertainty is insensitive to vertical displacements of the reference
level within the depth range between 800 and 2000 dbar.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
The occurrence of harmful epiphytic dinoflagellates is of concern to scientists, the aquaculture industry, and government
due to their toxicity not only to marine organisms but also to humans. There have been no studies on the abundance of the
epiphytic dinoflagellates in Korean waters. We explored the presence of epiphytic dinoflagellates in the coastal waters off
Jeju Island, southwestern Korea. Furthermore, we measured the abundance of epiphytic dinoflagellates on the thalli of 24 different
macroalgae, collected from five different locations in October 2009. Five epiphytic dinoflagellate genera Amphidinium, Coolia, Gambierdiscus, Ostreopsis, and Prorocentrum were found. These five genera were observed on the thalli of the macroalgae Chordaria flagelliformis, Martensia sp., Padina arborescens, and Sargassum sp., while none were observed exceptionally on Codium fragile. The abundance of Ostreopsis spp. was highest on Derbesia sp. (8,660 cells/g wet weight), while that of Gambierdiscus spp. was highest on Martensia sp. (4,870 cells/g-ww). The maximum abundances of Amphidinium spp., Coolia spp., and Prorocentrum spp. were 410, 710, and 300 cells/g-ww, respectively. The maximum abundance of Coolia spp., Gambierdiscus spp., and Ostreopsis spp. obtained in the present study was lower than for other locations reported in literature. The results of the present
study suggest that the presence and abundance of epiphytic dinoflagellates may be related to the macroalgal species of the
coastal waters of Jeju Island. 相似文献