Adopting drought indices for estimating soil moisture: A North Carolina case study

被引:107
作者
Sims, AP [1 ]
Niyogi, DDS [1 ]
Raman, S [1 ]
机构
[1] N Carolina State Univ, State Climate Off N Carolina, Raleigh, NC 27695 USA
关键词
D O I
10.1029/2001GL013343
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
[1] Soil moisture availability has a significant impact on environmental processes of different scales. Errors in initializing soil moisture in numerical weather forecasting models tend to cause errors in short-term weather and medium range predictions. We study the use of two drought indices: Palmer Drought Severity Index (PDSI) values and Standardized Precipitation Index (SPI) for estimating soil moisture. SPI and PDSI values are compared for three climate divisions: western mountains, central piedmont, and the coastal plain in North Carolina, USA. Results suggest SPI to be more representative of short-term precipitation and soil moisture variation and hence a better indicator of soil wetness. A regression equation that uses SPI is proposed to estimate soil moisture.
引用
收藏
页数:4
相关论文
共 18 条
[1]   Uncertainty in the specification of surface characteristics: A study of prediction errors in the boundary layer [J].
Alapaty, K ;
Raman, S ;
Niyogi, DS .
BOUNDARY-LAYER METEOROLOGY, 1997, 82 (03) :473-500
[2]  
ALLEY WM, 1984, J CLIM APPL METEOROL, V23, P1100, DOI 10.1175/1520-0450(1984)023<1100:TPDSIL>2.0.CO
[3]  
2
[4]  
Edwards E. C., 1997, 634 COL STAT U
[5]  
GUTTMAN NB, 1992, WATER RESOUR BULL, V28, P1111
[6]  
Heddinghaus T. R., 1991, P 7 C APPL CLIM, P242, DOI DOI 10.3996/012015-JFWM-001.S7
[7]  
Hu Q, 2000, INT J CLIMATOL, V20, P1899, DOI 10.1002/1097-0088(200012)20:15&lt
[8]  
1899::AID-JOC588&gt
[9]  
3.0.CO
[10]  
2-M