Analysis of the latest satellite rainfall and reanalysis datasets from 1998 to 2012 demonstrates that eastwardpropagating rainfall episodes, which typically occur in late night and morning, are determinant factors for the rainfall diurnal cycle and climate anomalies over eastern China. The episode growth and propagation are facilitated by an elevated layer of conditionally unstable air in a mesoscale zone at their eastern leading edge. The convective available potential energy (CAPE), despite convection consumption and nocturnal cooling, decreases only from a high value to a moderate one during episode duration. An estimate of the CAPE generation budget suggests that low-level horizontal advection and vertical lifting of the warm moist air can produce sufficient CAPE to balance other stabilization effects, sustaining the mesoscale maximum of convective instability ahead of rainfall episodes. These instability geneses are pronounced at the convection growth stage and linked closely to a mesoscale nocturnal low-level jet. Thus, a proper representation of them in forecast models is essential for improved prediction of the warm-season rainfall.
[1] We evaluated the impacts of historical land-use changes (LUCs) from 1987 to 2006 on surface warming rates and rice yields on the island of Shikoku, Japan. We performed two types of numerical simulations (with historical LUCs and with fixed land uses) using a regional atmospheric model (JMA-NHM) and a large-area rice-growth model (PRYSBI). During our study period in Shikoku, the area of paddy fields decreased markedly and the area of building lots and roads increased. Our evaluation suggests that these LUCs caused warming rates in and around paddy fields that were five times those in and around other land uses. The simulated rice yield in 2006 was 0.27% lower (0.012 t ha À1 ) than in 1987 in response to the change in thermal and solar radiation conditions. These results suggest that decreases of crop yield due to environmental deterioration will be found in other regions where similar LUCs are occurring. Citation: Yoshida, R., T. Iizumi, M. Nishimori, and M. Yokozawa (2012), Impacts of land-use changes on surface warming rates and rice yield in Shikoku, western Japan, Geophys. Res. Lett., 39, L22401,
SUMMARYObjective: To investigate whether the magnetoencephalography (MEG) single moving dipole (SMD) method could delineate the epileptic zone of focal cortical dysplasia (FCD) at the bottom of sulcus (FCDB). Methods: We retrospectively analyzed 17 children (11 male; mean age 8.8 years, range 3-17 years) with FCD type II who underwent epilepsy surgery. We compared spatial congruence between the following: (1) MEG cluster and FCDB and (2) MEG cluster and FCD at the brain surface (FCDS). We measured the volume and depth of magnetic resonance imaging (MRI)-visible lesions to investigate whether they affect spatial congruence between MEG cluster and MRI-visible lesion. Results: Eight children had FCDB and the other nine children had FCDS. ). There was a tendency for a smaller volume of MRI-visible lesion for FCDB, relative to FCDS(p = 0.079). In FCDB, six children showed clusters of MEG dipoles and two children showed scattered MEG dipoles for interictal spikes. The spatial congruence between the MEG result and FCDB was partially overlapping in four children and discordant in another four children. In FCDS, eight children had MEG cluster and one child had MEG scatter alone. The spatial congruence between MEG result and FCDS was overlapping in eight of nine children (fully two; partially six) and discordant in one of nine children. Fifteen children (88%; FCDB eight; FCDS seven) became seizure-free after resective surgery. MEG spike dipole resection ratio in the cluster ranged from 4-100% (mean 67%) in 6 FCDB and 23-99% (mean 77%) in 8 FCDS. Significance: The SMD method may drift MEG spike dipoles for FCDB. Lesionectomy can control seizures for four of eight patients in FCDB despite the remote MEG dipoles. The FCDB or FCDS partially overlapped with MEG cluster may have an extending/invisible epileptogenic zone consecutive to the MRI-visible lesion.
Background Heat stroke treatment focuses on rapid cooling because symptom severity correlates with the duration of hyperthermia (i.e., time during which the core body temperature is sustained above the critical threshold). Several reports have revealed that cold‐water immersion is a safe and appropriate therapy for exertional heat stroke in young, otherwise healthy patients. However, few reports have assessed cold‐water immersion in older patients. We document three cases of cold‐water immersion in older heat stroke patients and evaluate its safety and efficacy. Case presentation Three older patients with severe heat stroke were treated with cold‐water immersion. Core body temperatures decreased rapidly, and no complications occurred during the treatment. Conclusion Cold‐water immersion can achieve rapid cooling and is effective in treating heat stroke. With special precautions, it can be performed safely for older patients. Further investigation is warranted to establish appropriate cooling methods in older adults.
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