Asset Details
Do you wish to reserve the book?
2019年2月北京地区3次回流降雪过程的水汽输送特征分析
Hey, we have placed the reservation for you!
By the way, why not check out events that you can attend while you pick your title.
Oops! Something went wrong.
Looks like we were not able to place the reservation. Kindly try again later.
Are you sure you want to remove the book from the shelf?
2019年2月北京地区3次回流降雪过程的水汽输送特征分析
Do you wish to request the book?
2019年2月北京地区3次回流降雪过程的水汽输送特征分析
Please be aware that the book you have requested cannot be checked out. If you would like to checkout this book, you can reserve another copy
We have requested the book for you!
Your request is successful and it will be processed during the Library working hours. Please check the status of your request in My Requests.
Oops! Something went wrong.
Looks like we were not able to place your request. Kindly try again later.
Journal Article
2019年2月北京地区3次回流降雪过程的水汽输送特征分析
2024
Overview
为提高北京地区回流降雪预报的准确率,利用ERA5/GDAS全球格点再分析资料和HYSPLIT轨迹追踪模式,对2019年2月发生在北京地区的3次回流降雪过程进行天气学分析和水汽输送特征分析.结果表明,在3次回流降雪个例中,偏东气流中的水汽含量有限,当出现偏南水汽通道的配合时,可产生明显的降雪.在典型回流形势(2月14日)下,高后回流与河套倒槽配合,回流水汽输送通道更为深厚,利于降雪;在非典型回流形势(2月6日和12日)下,回流水汽输送集中于大气的低层(850 hPa以下).2月12日南支气流水汽输送贡献较大,对南支气流水汽输送的忽视是导致2月12日降雪漏报的原因之一.3次回流降雪个例在偏东和偏南路径上水汽输送至北京地区的时间与白天显著降雪的时段基本上对应,可作为预报回流降雪的关键因子.
Publisher
北京大学物理学院大气与海洋科学系,北京 100871
We currently cannot retrieve any items related to this title. Kindly check back at a later time.