Estimating the temperature of a maize apex during early growth stages
When the leaf area index is low at the early stages of growth, the temperature of a maize apex can be much higher than the air temperature measured at screen level. In order to account for temperature effects in plant growth simulation models, it would be better to use plant temperature rather than...
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Veröffentlicht in: | Agricultural and forest meteorology 1993-02, Vol.63 (1), p.35-54 |
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description | When the leaf area index is low at the early stages of growth, the temperature of a maize apex can be much higher than the air temperature measured at screen level. In order to account for temperature effects in plant growth simulation models, it would be better to use plant temperature rather than air temperature. We propose a model to estimate the apex temperature for both day-time and night-time averages from a small number of readily available meteorological data: solar radiation, wind speed, air temperature and humidity. It is based on an energy balance of a maize apex under field conditions. It performs a radiation balance that separates diffuse and direct components, and assumes a similarity between the apex and soil surface temperature evolutions. In the absence of any references, the apex stomatal resistance was parameterized as a simple linear function of water vapour deficit, deduced from experimental data. The calculated temperatures were compared with those measured for two sets of experimental data collected in 1989 and 1990. The agreement was quite satisfactory, the average absolute error being in all cases less than 1.0°C. Furthermore, the empirical relationship between stomatal resistance and water vapour deficit was shown to be valid for both sets of data. We should now confirm this relation under different soil or climatic conditions, as well as the similarity between the apex and soil surface temperatures. |
doi_str_mv | 10.1016/0168-1923(93)90021-9 |
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In order to account for temperature effects in plant growth simulation models, it would be better to use plant temperature rather than air temperature. We propose a model to estimate the apex temperature for both day-time and night-time averages from a small number of readily available meteorological data: solar radiation, wind speed, air temperature and humidity. It is based on an energy balance of a maize apex under field conditions. It performs a radiation balance that separates diffuse and direct components, and assumes a similarity between the apex and soil surface temperature evolutions. In the absence of any references, the apex stomatal resistance was parameterized as a simple linear function of water vapour deficit, deduced from experimental data. The calculated temperatures were compared with those measured for two sets of experimental data collected in 1989 and 1990. The agreement was quite satisfactory, the average absolute error being in all cases less than 1.0°C. 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Plant production ; GROWTH ; LEAF AREA ; Life Sciences ; METEOROLOGICAL ELEMENTS ; MICROCLIMA ; MICROCLIMAT ; MICROCLIMATE ; MODELE DE SIMULATION ; MODELOS DE SIMULACION ; Silviculture, forestry ; SIMULATION MODELS ; STOMATA ; STOMATE ; SUPERFICIE FOLIAR ; SURFACE FOLIAIRE ; TEMPERATURA ; TEMPERATURE ; VAPEUR D'EAU ; VAPOR DE AGUA ; WATER VAPOUR ; ZEA MAYS</subject><ispartof>Agricultural and forest meteorology, 1993-02, Vol.63 (1), p.35-54</ispartof><rights>1993</rights><rights>1993 INIST-CNRS</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c388t-7dc2826ace8886fec0c9e8e6745fd8b8e36db1f2fbc03c0fe945880413a011963</citedby><cites>FETCH-LOGICAL-c388t-7dc2826ace8886fec0c9e8e6745fd8b8e36db1f2fbc03c0fe945880413a011963</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/0168192393900219$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>230,314,776,780,881,3537,27901,27902,65306</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=4529867$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://hal.inrae.fr/hal-02700598$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Cellier, P.</creatorcontrib><creatorcontrib>Ruget, F.</creatorcontrib><creatorcontrib>Chartier, M.</creatorcontrib><creatorcontrib>Bonhomme, R.</creatorcontrib><title>Estimating the temperature of a maize apex during early growth stages</title><title>Agricultural and forest meteorology</title><description>When the leaf area index is low at the early stages of growth, the temperature of a maize apex can be much higher than the air temperature measured at screen level. In order to account for temperature effects in plant growth simulation models, it would be better to use plant temperature rather than air temperature. We propose a model to estimate the apex temperature for both day-time and night-time averages from a small number of readily available meteorological data: solar radiation, wind speed, air temperature and humidity. It is based on an energy balance of a maize apex under field conditions. It performs a radiation balance that separates diffuse and direct components, and assumes a similarity between the apex and soil surface temperature evolutions. In the absence of any references, the apex stomatal resistance was parameterized as a simple linear function of water vapour deficit, deduced from experimental data. The calculated temperatures were compared with those measured for two sets of experimental data collected in 1989 and 1990. The agreement was quite satisfactory, the average absolute error being in all cases less than 1.0°C. Furthermore, the empirical relationship between stomatal resistance and water vapour deficit was shown to be valid for both sets of data. We should now confirm this relation under different soil or climatic conditions, as well as the similarity between the apex and soil surface temperatures.</description><subject>Agricultural and forest climatology and meteorology. Irrigation. Drainage</subject><subject>Agricultural and forest meteorology</subject><subject>Agricultural sciences</subject><subject>Agronomy. Soil science and plant productions</subject><subject>Biological and medical sciences</subject><subject>CONDICIONES ATMOSFERICAS</subject><subject>CONDITIONS METEOROLOGIQUES</subject><subject>CRECIMIENTO</subject><subject>CROISSANCE</subject><subject>Crop climate. Energy and radiation balances</subject><subject>ESTOMA</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>General agronomy. Plant production</subject><subject>GROWTH</subject><subject>LEAF AREA</subject><subject>Life Sciences</subject><subject>METEOROLOGICAL ELEMENTS</subject><subject>MICROCLIMA</subject><subject>MICROCLIMAT</subject><subject>MICROCLIMATE</subject><subject>MODELE DE SIMULATION</subject><subject>MODELOS DE SIMULACION</subject><subject>Silviculture, forestry</subject><subject>SIMULATION MODELS</subject><subject>STOMATA</subject><subject>STOMATE</subject><subject>SUPERFICIE FOLIAR</subject><subject>SURFACE FOLIAIRE</subject><subject>TEMPERATURA</subject><subject>TEMPERATURE</subject><subject>VAPEUR D'EAU</subject><subject>VAPOR DE AGUA</subject><subject>WATER VAPOUR</subject><subject>ZEA MAYS</subject><issn>0168-1923</issn><issn>1873-2240</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1993</creationdate><recordtype>article</recordtype><recordid>eNp9kE1LAzEQhoMoWKt_QDzk4MEeVvOx3U0ugki1QtGLnsM0O2kjbbckqV-_3iwrPQoJGTLPOwwPIRecXXPGq5t8VcG1kFdajjRjghf6gAy4qmUhRMkOyWCPHJOTGN8Z46Ku9YBMJjH5NSS_WdC0RJpwvcUAaReQto4CXYP_QQpb_KLNLnQYQlh900VoP9OSxgQLjKfkyMEq4tnfOyRvD5PX-2kxe3l8ur-bFVYqlYq6sUKJCiwqpSqHllmNCqu6HLtGzRXKqplzJ9zcMmmZQ12OlWIll8A415UcklE_dwkrsw158fBtWvBmejcz3R8TNWNjrT54ZsuetaGNMaDbBzgznTbTOTGdE6Pz6bTlYkgu-9gWooWVC7CxPu6z5VhoVdUZO-8xB62BRcjI80zLPJLL3Lztm5hdfHgMJlqPG4uND2iTaVr__xK_9PKIDQ</recordid><startdate>19930201</startdate><enddate>19930201</enddate><creator>Cellier, P.</creator><creator>Ruget, F.</creator><creator>Chartier, M.</creator><creator>Bonhomme, R.</creator><general>Elsevier B.V</general><general>Elsevier</general><general>Elsevier Masson</general><scope>FBQ</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>1XC</scope></search><sort><creationdate>19930201</creationdate><title>Estimating the temperature of a maize apex during early growth stages</title><author>Cellier, P. ; Ruget, F. ; Chartier, M. ; Bonhomme, R.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c388t-7dc2826ace8886fec0c9e8e6745fd8b8e36db1f2fbc03c0fe945880413a011963</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1993</creationdate><topic>Agricultural and forest climatology and meteorology. Irrigation. Drainage</topic><topic>Agricultural and forest meteorology</topic><topic>Agricultural sciences</topic><topic>Agronomy. Soil science and plant productions</topic><topic>Biological and medical sciences</topic><topic>CONDICIONES ATMOSFERICAS</topic><topic>CONDITIONS METEOROLOGIQUES</topic><topic>CRECIMIENTO</topic><topic>CROISSANCE</topic><topic>Crop climate. Energy and radiation balances</topic><topic>ESTOMA</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>General agronomy. Plant production</topic><topic>GROWTH</topic><topic>LEAF AREA</topic><topic>Life Sciences</topic><topic>METEOROLOGICAL ELEMENTS</topic><topic>MICROCLIMA</topic><topic>MICROCLIMAT</topic><topic>MICROCLIMATE</topic><topic>MODELE DE SIMULATION</topic><topic>MODELOS DE SIMULACION</topic><topic>Silviculture, forestry</topic><topic>SIMULATION MODELS</topic><topic>STOMATA</topic><topic>STOMATE</topic><topic>SUPERFICIE FOLIAR</topic><topic>SURFACE FOLIAIRE</topic><topic>TEMPERATURA</topic><topic>TEMPERATURE</topic><topic>VAPEUR D'EAU</topic><topic>VAPOR DE AGUA</topic><topic>WATER VAPOUR</topic><topic>ZEA MAYS</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Cellier, P.</creatorcontrib><creatorcontrib>Ruget, F.</creatorcontrib><creatorcontrib>Chartier, M.</creatorcontrib><creatorcontrib>Bonhomme, R.</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Hyper Article en Ligne (HAL)</collection><jtitle>Agricultural and forest meteorology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Cellier, P.</au><au>Ruget, F.</au><au>Chartier, M.</au><au>Bonhomme, R.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Estimating the temperature of a maize apex during early growth stages</atitle><jtitle>Agricultural and forest meteorology</jtitle><date>1993-02-01</date><risdate>1993</risdate><volume>63</volume><issue>1</issue><spage>35</spage><epage>54</epage><pages>35-54</pages><issn>0168-1923</issn><eissn>1873-2240</eissn><coden>AFMEEB</coden><abstract>When the leaf area index is low at the early stages of growth, the temperature of a maize apex can be much higher than the air temperature measured at screen level. In order to account for temperature effects in plant growth simulation models, it would be better to use plant temperature rather than air temperature. We propose a model to estimate the apex temperature for both day-time and night-time averages from a small number of readily available meteorological data: solar radiation, wind speed, air temperature and humidity. It is based on an energy balance of a maize apex under field conditions. It performs a radiation balance that separates diffuse and direct components, and assumes a similarity between the apex and soil surface temperature evolutions. In the absence of any references, the apex stomatal resistance was parameterized as a simple linear function of water vapour deficit, deduced from experimental data. The calculated temperatures were compared with those measured for two sets of experimental data collected in 1989 and 1990. The agreement was quite satisfactory, the average absolute error being in all cases less than 1.0°C. Furthermore, the empirical relationship between stomatal resistance and water vapour deficit was shown to be valid for both sets of data. We should now confirm this relation under different soil or climatic conditions, as well as the similarity between the apex and soil surface temperatures.</abstract><cop>Amsterdam</cop><cop>Oxford</cop><cop>New York, NY</cop><pub>Elsevier B.V</pub><doi>10.1016/0168-1923(93)90021-9</doi><tpages>20</tpages></addata></record> |
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subjects | Agricultural and forest climatology and meteorology. Irrigation. Drainage Agricultural and forest meteorology Agricultural sciences Agronomy. Soil science and plant productions Biological and medical sciences CONDICIONES ATMOSFERICAS CONDITIONS METEOROLOGIQUES CRECIMIENTO CROISSANCE Crop climate. Energy and radiation balances ESTOMA Fundamental and applied biological sciences. Psychology General agronomy. Plant production GROWTH LEAF AREA Life Sciences METEOROLOGICAL ELEMENTS MICROCLIMA MICROCLIMAT MICROCLIMATE MODELE DE SIMULATION MODELOS DE SIMULACION Silviculture, forestry SIMULATION MODELS STOMATA STOMATE SUPERFICIE FOLIAR SURFACE FOLIAIRE TEMPERATURA TEMPERATURE VAPEUR D'EAU VAPOR DE AGUA WATER VAPOUR ZEA MAYS |
title | Estimating the temperature of a maize apex during early growth stages |
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