Search Results

You are looking at 1 - 2 of 2 items for :

  • Author or Editor: Yongkang Xue x
  • Bulletin of the American Meteorological Society x
  • Refine by Access: Content accessible to me x
Clear All Modify Search
Aaron Boone
,
Patricia de Rosnay
,
Gianpaolo Balsamo
,
Anton Beljaars
,
Franck Chopin
,
Bertrand Decharme
,
Christine Delire
,
Agnes Ducharne
,
Simon Gascoin
,
Manuela Grippa
,
Françoise Guichard
,
Yeugeniy Gusev
,
Phil Harris
,
Lionel Jarlan
,
Laurent Kergoat
,
Eric Mougin
,
Olga Nasonova
,
Anette Norgaard
,
Tristan Orgeval
,
Catherine Ottlé
,
Isabelle Poccard-Leclercq
,
Jan Polcher
,
Inge Sandholt
,
Stephane Saux-Picart
,
Christopher Taylor
, and
Yongkang Xue

The rainfall over West Africa has been characterized by extreme variability in the last half-century, with prolonged droughts resulting in humanitarian crises. There is, therefore, an urgent need to better understand and predict the West African monsoon (WAM), because social stability in this region depends to a large degree on water resources. The economies are primarily agrarian, and there are issues related to food security and health. In particular, there is a need to better understand land-atmosphere and hydrological processes over West Africa because of their potential feedbacks with the WAM. This is being addressed through a multiscale modeling approach using an ensemble of land surface models that rely on dedicated satellite-based forcing and land surface parameter products, and data from the African Multidisciplinary Monsoon Analysis (AMMA) observational field campaigns. The AMMA land surface model (LSM) Intercomparison Project (ALMIP) offline, multimodel simulations comprise the equivalent of a multimodel reanalysis product. They currently represent the best estimate of the land surface processes over West Africa from 2004 to 2007. An overview of model intercomparison and evaluation is presented. The far-reaching goal of this effort is to obtain better understanding and prediction of the WAM and the feedbacks with the surface. This can be used to improve water management and agricultural practices over this region.

Full access
Tandong Yao
,
Yongkang Xue
,
Deliang Chen
,
Fahu Chen
,
Lonnie Thompson
,
Peng Cui
,
Toshio Koike
,
William K.-M. Lau
,
Dennis Lettenmaier
,
Volker Mosbrugger
,
Renhe Zhang
,
Baiqing Xu
,
Jeff Dozier
,
Thomas Gillespie
,
Yu Gu
,
Shichang Kang
,
Shilong Piao
,
Shiori Sugimoto
,
Kenichi Ueno
,
Lei Wang
,
Weicai Wang
,
Fan Zhang
,
Yongwei Sheng
,
Weidong Guo
,
Ailikun
,
Xiaoxin Yang
,
Yaoming Ma
,
Samuel S. P. Shen
,
Zhongbo Su
,
Fei Chen
,
Shunlin Liang
,
Yimin Liu
,
Vijay P. Singh
,
Kun Yang
,
Daqing Yang
,
Xinquan Zhao
,
Yun Qian
,
Yu Zhang
, and
Qian Li

Abstract

The Third Pole (TP) is experiencing rapid warming and is currently in its warmest period in the past 2,000 years. This paper reviews the latest development in multidisciplinary TP research associated with this warming. The rapid warming facilitates intense and broad glacier melt over most of the TP, although some glaciers in the northwest are advancing. By heating the atmosphere and reducing snow/ice albedo, aerosols also contribute to the glaciers melting. Glacier melt is accompanied by lake expansion and intensification of the water cycle over the TP. Precipitation has increased over the eastern and northwestern TP. Meanwhile, the TP is greening and most regions are experiencing advancing phenological trends, although over the southwest there is a spring phenological delay mainly in response to the recent decline in spring precipitation. Atmospheric and terrestrial thermal and dynamical processes over the TP affect the Asian monsoon at different scales. Recent evidence indicates substantial roles that mesoscale convective systems play in the TP’s precipitation as well as an association between soil moisture anomalies in the TP and the Indian monsoon. Moreover, an increase in geohazard events has been associated with recent environmental changes, some of which have had catastrophic consequences caused by glacial lake outbursts and landslides. Active debris flows are growing in both frequency of occurrences and spatial scale. Meanwhile, new types of disasters, such as the twin ice avalanches in Ali in 2016, are now appearing in the region. Adaptation and mitigation measures should be taken to help societies’ preparation for future environmental challenges. Some key issues for future TP studies are also discussed.

Full access