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


     


Published online 11 May 2007
Published in Agron J 99:862-866 (2007)
DOI: 10.2134/agronj2006.0264
© 2007 American Society of Agronomy
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Abstract Freely available
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 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 Forcella, F.
Right arrow Articles by Weyers, S. L.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Forcella, F.
Right arrow Articles by Weyers, S. L.
Agricola
Right arrow Articles by Forcella, F.
Right arrow Articles by Weyers, S. L.
Related Collections
Right arrow Agroclimatology
Right arrow Best Management Practices
Right arrow Nutrient Management

Mid-Continent Fall Temperatures at the 10-cm Soil Depth

Frank Forcella* and Sharon Lachnicht Weyers

USDA-ARS, North Central Soil Conservation Research Lab., 803 Iowa Ave., Morris, MN 56267


Figure 1
View larger version (18K):
[in this window]
[in a new window]

 
Fig. 1. Average daily soil temperatures at 10-cm depth from Grand Forks, ND, during autumn in 1999 and 2003. In 1999, once soil temperature dropped below 10°C, it stayed low for the remainder of the cold season, which is the desired scenario for fall-applied nitrogen fertilizer. In contrast, in 2003, after first dropping below 10°C, soil temperature rose above this level three times, which possibly enhanced nitrogen losses.

 

Figure 2
View larger version (38K):
[in this window]
[in a new window]

 
Fig. 2. Locations of sites from which soil temperature data were recorded and analyzed.

 

Figure 3
View larger version (20K):
[in this window]
[in a new window]

 
Fig. 3. Average dates (±SD) of the first day in autumn that soil temperature at 10-cm depth dropped below 10°C and the last day in autumn that soil temperature exceeded 10°C. Data are for 26 sites with weather stations along a north-south transect between 36° and 49° N latitude, approximating the mid-continent of the USA.

 

Figure 4
View larger version (20K):
[in this window]
[in a new window]

 
Fig. 4. (A) Average ranges of days between the first day in autumn that soil temperature at 10-cm depth dropped below 10°C (First10) and the last day in autumn that soil temperature exceeded 10°C (Last10) among 26 weather stations along a latitudinal transect. (B) Coefficients of variation associated with averages in Fig. 4A.

 

Figure 5
View larger version (30K):
[in this window]
[in a new window]

 
Fig. 5. (A) Cumulative number of days between the first day in autumn that soil temperature at 10-cm depth dropped below 10°C (First10) and the last day in autumn that soil temperature exceeded 10°C (Last10) during which average daily soil temperature at 10-cm depth exceeded 10°C along a latitudinal transect of weather stations. (B) Cumulative degree-days (base 10°C) associated with Fig. 4A.

 





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 © 2007 by the American Society of Agronomy.