Agronomy Journal Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published online 19 October 2005
Published in Agron J 97:1478-1484 (2005)
DOI: 10.2134/agronj2004.0227
© 2005 American Society of Agronomy
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Figures Only
Right arrow Full Text Free
Right arrow Full Text (PDF) Free
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Hubbard, K. G.
Right arrow Articles by Wu, H.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Hubbard, K. G.
Right arrow Articles by Wu, H.
Agricola
Right arrow Articles by Hubbard, K. G.
Right arrow Articles by Wu, H.
Related Collections
Right arrow Agroclimatology
Right arrow Maize
Right arrow Crop Models

Agroclimatology

Modification of a Crop-Specific Drought Index for Simulating Corn Yield in Wet Years

Kenneth G. Hubbarda,* and Hong Wua,b

a High Plains Regional Climate Center, Univ. of Nebraska, Lincoln, NE 68583-0728
b Current address: Texas Inst. for Appl. Environ. Res., Tarleton State Univ., Stephenville, TX 76402

* Corresponding author (khubbard1{at}unl.edu)

Received for publication August 27, 2004. Drought occurs when there is a deficit in soil water supply to the plant. Severe drought limits crop yield by causing the plant's water use to be limited compared with a well-watered crop. Too much water (flooded soils) also causes stress to the plant whose roots are in saturated soil for long periods. Both situations lead to crop water stress, ultimately resulting in reduced crop yield. Since flood and drought can occur intermittently in cropping, an effective yield predictor should contain both flood and drought stress components for better representation of the range of natural conditions the plant might encounter during its growth period. This paper details the modification of the Crop-Specific Drought Index (CSDI) model by introducing a soil saturation factor, resulting in a Crop-Specific Stress Index (CSSI) model. The study was conducted in eastern Nebraska and southeastern Minnesota. The coefficients used in the CSSI model were estimated by a jackknifing procedure based on 1971–2002 climate data, nonirrigated yield data of corn (Zea mays L.), and soil information retrieved from the STATSGO database in the crop districts. Results show that all indicators of agreement between the estimated and actual yields show improvement of the new CSSI model over the old CSDI model in all districts. Results also show that the CSSI model outperforms the CSDI model in years characterized by soil saturation. For instance, the CSDI for 1993 overestimates the relative yield in northeastern Nebraska by about 28% while the CSSI underestimates the 1993 yield by 3%.

Abbreviations: COOP, Cooperative Weather Station Network • CSDI, Crop-Specific Drought Index • CSSI, Crop-Specific Stress Index • ET, evapotranspiration • RMSE, root mean square errors • STATSGO, State Soil Geographic database







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Crop Science Vadose Zone Journal
Journal of Natural Resources
and Life Sciences Education
Soil Science Society of America Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2005 by the American Society of Agronomy.