TY  - JOUR
A1  - Gerlitz, Lars
A1  - Steirou, Eva
A1  - Schneider, Christoph
A1  - Moron, Vincent
A1  - Vorogushyn, Sergiy
A1  - Merz, Bruno
T1  - Variability of the Cold Season Climate in Central Asia. Part II: Hydroclimatic Predictability
JF  - Journal of climate
N2  - Central Asia (CA) is subjected to a large variability of precipitation. This study presents a statistical model, relating precipitation anomalies in three subregions of CA in the cold season (November-March) with various predictors in the preceding October. Promising forecast skill is achieved for two subregions covering 1) Uzbekistan, Turkmenistan, Kyrgyzstan, Tajikistan, and southern Kazakhstan and 2) Iran, Afghanistan, and Pakistan. ENSO in October is identified as the major predictor. Eurasian snow cover and the quasi-biennial oscillation further improve the forecast performance. To understand the physical mechanisms, an analysis of teleconnections between these predictors and the wintertime circulation over CA is conducted. The correlation analysis of predictors and large-scale circulation indices suggests a seasonal persistence of tropical circulation modes and a dynamical forcing of the westerly circulation by snow cover variations over Eurasia. An EOF analysis of pressure and humidity patterns allows separating the circulation variability over CA into westerly and tropical modes and confirms that the identified predictors affect the respective circulation characteristics. Based on the previously established weather type classification for CA, the predictors are investigated with regard to their effect on the regional circulation. The results suggest a modification of the Hadley cell due to ENSO variations, with enhanced moisture supply from the Arabian Gulf during El Nino. They further indicate an influence of Eurasian snow cover on the wintertime Arctic Oscillation (AO) and Northern Hemispheric Rossby wave tracks. Positive anomalies favor weather types associated with dry conditions, while negative anomalies promote the formation of a quasi-stationary trough over CA, which typically occurs during positive AO conditions.
KW  - Asia
KW  - Climate prediction
KW  - Seasonal forecasting
KW  - North Atlantic Oscillation
KW  - Southern Oscillation
Y1  - 2019
U6  - https://doi.org/10.1175/JCLI-D-18-0892.1
SN  - 0894-8755
SN  - 1520-0442
VL  - 32
IS  - 18
SP  - 6015
EP  - 6033
PB  - American Meteorological Soc.
CY  - Boston
ER  -