Land surface phenologies and seasonalities using cool earthlight in mid-latitude croplands

Phenology deals with timing of biotic phenomena and seasonality concerns temporal patterns of abiotic variables. Studies of land surface phenology (LSP) and land surface seasonality (LSS) have long been limited to visible to near infrared (VNIR) wavelengths, despite degradation by atmospheric effect...

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Main Authors: W G Alemu, G M Henebry
Format: Article
Language:English
Published: IOP Publishing 2013-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/8/4/045002
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author W G Alemu
G M Henebry
author_facet W G Alemu
G M Henebry
author_sort W G Alemu
collection DOAJ
description Phenology deals with timing of biotic phenomena and seasonality concerns temporal patterns of abiotic variables. Studies of land surface phenology (LSP) and land surface seasonality (LSS) have long been limited to visible to near infrared (VNIR) wavelengths, despite degradation by atmospheric effects and solar illumination constraints. Enhanced land surface parameters derived from passive microwave data enable improved temporal monitoring of agricultural land surface dynamics compared to the vegetation index data available from VNIR data. LSPs and LSSs in grain growing regions of the Volga River Basin of Russia and the spring wheat belts of the USA and Canada were characterized using AMSR-E enhanced land surface parameters for the period from April through October for 2003 through 2010. Growing degree-days (GDDs) were calculated from AMSR-E air temperature retrievals using both ascending and descending passes with a base of 0 ° C and then accumulated (AGDD) with an annual restart each 1 April. Tracking the AMSR-E parameters as a function of AGDD revealed the expected seasonal pattern of thermal limitation in mid-latitude croplands. Vegetation optical depth (VOD), a microwave analog of a vegetation index, was modeled as a function of AGDD with the resulting fitted convex quadratic models yielding both high coefficients of determination ( r ^2  > 0.90) and phenometrics that could characterize cropland differences between the Russian and North American sites. The AMSR-E data were also able to capture the effects of the 2010 heat wave that devastated grain production in European Russia. These results showed the potential of AMSR-E in monitoring and modeling cropland dynamics.
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spelling doaj.art-34ecc10b45714521beced92cfcd8cd4a2023-08-09T14:42:58ZengIOP PublishingEnvironmental Research Letters1748-93262013-01-018404500210.1088/1748-9326/8/4/045002Land surface phenologies and seasonalities using cool earthlight in mid-latitude croplandsW G Alemu0G M Henebry1Geospatial Sciences Center of Excellence, South Dakota State University , 1021 Medary Avenue, Wecota Hall 506B, Brookings, SD 57007-3510, USAGeospatial Sciences Center of Excellence, South Dakota State University , 1021 Medary Avenue, Wecota Hall 506B, Brookings, SD 57007-3510, USAPhenology deals with timing of biotic phenomena and seasonality concerns temporal patterns of abiotic variables. Studies of land surface phenology (LSP) and land surface seasonality (LSS) have long been limited to visible to near infrared (VNIR) wavelengths, despite degradation by atmospheric effects and solar illumination constraints. Enhanced land surface parameters derived from passive microwave data enable improved temporal monitoring of agricultural land surface dynamics compared to the vegetation index data available from VNIR data. LSPs and LSSs in grain growing regions of the Volga River Basin of Russia and the spring wheat belts of the USA and Canada were characterized using AMSR-E enhanced land surface parameters for the period from April through October for 2003 through 2010. Growing degree-days (GDDs) were calculated from AMSR-E air temperature retrievals using both ascending and descending passes with a base of 0 ° C and then accumulated (AGDD) with an annual restart each 1 April. Tracking the AMSR-E parameters as a function of AGDD revealed the expected seasonal pattern of thermal limitation in mid-latitude croplands. Vegetation optical depth (VOD), a microwave analog of a vegetation index, was modeled as a function of AGDD with the resulting fitted convex quadratic models yielding both high coefficients of determination ( r ^2  > 0.90) and phenometrics that could characterize cropland differences between the Russian and North American sites. The AMSR-E data were also able to capture the effects of the 2010 heat wave that devastated grain production in European Russia. These results showed the potential of AMSR-E in monitoring and modeling cropland dynamics.https://doi.org/10.1088/1748-9326/8/4/045002microwavesphenologyremote sensingAMSR-Econvex quadratic modelEuropean Russia
spellingShingle W G Alemu
G M Henebry
Land surface phenologies and seasonalities using cool earthlight in mid-latitude croplands
Environmental Research Letters
microwaves
phenology
remote sensing
AMSR-E
convex quadratic model
European Russia
title Land surface phenologies and seasonalities using cool earthlight in mid-latitude croplands
title_full Land surface phenologies and seasonalities using cool earthlight in mid-latitude croplands
title_fullStr Land surface phenologies and seasonalities using cool earthlight in mid-latitude croplands
title_full_unstemmed Land surface phenologies and seasonalities using cool earthlight in mid-latitude croplands
title_short Land surface phenologies and seasonalities using cool earthlight in mid-latitude croplands
title_sort land surface phenologies and seasonalities using cool earthlight in mid latitude croplands
topic microwaves
phenology
remote sensing
AMSR-E
convex quadratic model
European Russia
url https://doi.org/10.1088/1748-9326/8/4/045002
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