Ocean Research Institute, University of Tokyo, Tokyo, JapanSpringer NetherlandsJournal of the Oceanographical Society of JapanMaeda, A. (1971), Changes of water temperature near ocean weather sta- tion T before and after passage of a typhoon, J. Oceanogr. Soc. Jpn., 27, 109-115, doi:10.1007/BF02109766.
our understanding of the influence of climate on tropical cyclone behaviour is restricted by the short historical record and the sparseness of prehistorical reconstructions, particularly in the western North Pacific, where coastal communities
根据第一段“Small changes in atmospheric pressure can start a landslide in certain weather conditions. Understanding why will help us assess which slopes(斜坡) are at most risk of failing.(在某些天气条件下,大气压力的微小变化可能引发滑坡。了解其中的原因将有助于我们评估哪些斜坡最容易坍塌)”以及第...
Translation speed of TCs is one important feature because the slower TCs move, the longer is their influence time, and the greater is the impact of severe weather events associated with TCs such as heavy rain and strong winds1,2. In relation to the anticipated increase in precipitation ...
Average annual precipitation is 836.5 mm, according to the closest weather station in Ville Marie. The study area at the northern edge of the sugar maple–yellow birch bioclimatic domain of southwest- ern Quebec (Saucier et al. 1998), which is part of the broader Great Lakes-St. ...
stated that, at that time, the SAR government requested enterprises to ensure local employment; Sands China team members united to weather the storm together while remaining committed to helping society cope with the pandemic. Throughout it all, Sands China was full of confidence about Macau’s ...
Before 1960, the city population was almost equivalent to the DID population. Therefore, for 1940–1950, we derived the number of households in landslide-prone areas from the number of ordinary households (Section 2.3.5) and the populations of towns and villages; for 1960–2015, we derived ...
We have also identified periods of enhanced terrestrial particulate organic carbon transfer to the ocean driven by short-lived extreme events, most likely typhoons, during the Bølling–Allerød, at the beginning of the Early Holocene and the end of the Late Holocene, when the typhoon dynamics ...
weather events other than cyclones were quite small. Further analysis showed that the numbers of typhoons and extratropical cyclones affecting the studied region were projected to decrease by 40 and 15%, respectively, whereas the precipitation brought on by a single event, i.e. one typhoon or ...
In addition, model simulations were carried out using a series of 1-h interval precipitation data of rainfall events from weather stations in the Yunbei-Large-Encirclement Project area. 2.3 Methods 2.3.1 Assessing changes in characteristics of river system In order to quantitatively ...