Improvements in the Estimation of Air Temperature with Empirical Models on Livingston and Deception Islands in Maritime Antarctica (2000–2016) Using C6 MODIS LST

Guardado en:
Bibliografiske detaljer
Udgivet i:Remote Sensing vol. 16, no. 6 (2024), p. 1084
Hovedforfatter: Corbea-Pérez, Alejandro
Andre forfattere: Recondo, Carmen, Calleja, Javier F
Udgivet:
MDPI AG
Fag:
Online adgang:Citation/Abstract
Full Text + Graphics
Full Text - PDF
Tags: Tilføj Tag
Ingen Tags, Vær først til at tagge denne postø!

MARC

LEADER 00000nab a2200000uu 4500
001 3003409632
003 UK-CbPIL
022 |a 2072-4292 
024 7 |a 10.3390/rs16061084  |2 doi 
035 |a 3003409632 
045 2 |b d20240101  |b d20241231 
084 |a 231556  |2 nlm 
100 1 |a Corbea-Pérez, Alejandro  |u Department of Computer and Systems Engineering, University of La Laguna, Camino San Francisco de Paula, n19, 38200 San Cristóbal de La Laguna, Spain 
245 1 |a Improvements in the Estimation of Air Temperature with Empirical Models on Livingston and Deception Islands in Maritime Antarctica (2000–2016) Using C6 MODIS LST 
260 |b MDPI AG  |c 2024 
513 |a Journal Article 
520 3 |a Temperature analysis is of special interest in polar areas because temperature is an essential variable in the energy exchange between the Earth’s surface and atmosphere. Although land surface temperature (LST) obtained using satellites and air temperature (Ta) have different physical meanings and are measured with different techniques, LST has often been successfully employed to estimate Ta. For this reason, in this work, we estimated Ta from LST MODIS collection 6 (C6) and used other predictor variables. Daily mean Ta was calculated from Spanish State Meteorological Agency (AEMET) stations data on the Livingston and Deception Islands, and from the PERMASNOW project stations on Livingston Island; both islands being part of the South Shetland Islands (SSI) archipelago. In relation to our previous work carried out in the study area with collection 5 (C5) data, we obtained higher R2 values (R2CV = 0.8, in the unique model with Terra daytime data) and lower errors (RMSECV = 2.2 °C, MAECV = 1.6 °C). We corroborated significant improvements in MODIS C6 LST data. We analyzed emissivity as a possible factor of discrepancies between C5 and C6, but we did not find conclusive results, therefore we could not affirm that emissivity is the factor that causes differences between one collection and another. The results obtained with the applied filters indicated that MODIS data can be used to study Ta in the area, as these filters contribute to the reduction of uncertainties in the modeling of Ta from satellites. 
651 4 |a Livingston Island 
651 4 |a Antarctic Peninsula 
651 4 |a Deception Island 
651 4 |a Antarctica 
653 |a Earth surface 
653 |a Permafrost 
653 |a Emissivity 
653 |a Air temperature 
653 |a Empirical analysis 
653 |a Land surface temperature 
653 |a Satellites 
653 |a Filters 
653 |a Islands 
653 |a Radiation 
653 |a Ice 
653 |a Climate change 
653 |a Archipelagoes 
653 |a Atmospheric models 
653 |a Sensors 
653 |a MODIS 
653 |a Variables 
653 |a Climate science 
653 |a Deception 
653 |a Statistical methods 
700 1 |a Recondo, Carmen  |u Remote Sensing Applications (RSApps) Research Group, Area of Cartographic, Geodesic and Photogrammetric Engineering, Department of Mining Exploitation and Prospecting, Polytechnic School of Mieres, University of Oviedo, C/Gonzalo Gutiérrez Quirós s/n, 33600 Mieres, Spain; <email>mdrecondo@uniovi.es</email> 
700 1 |a Calleja, Javier F  |u Remote Sensing Applications (RSApps) Research Group, Department of Physics, Polytechnic School of Mieres, University of Oviedo, C/Gonzalo Gutiérrez Quirós s/n, 33600 Mieres, Spain; <email>jfcalleja@uniovi.es</email> 
773 0 |t Remote Sensing  |g vol. 16, no. 6 (2024), p. 1084 
786 0 |d ProQuest  |t Advanced Technologies & Aerospace Database 
856 4 1 |3 Citation/Abstract  |u https://www.proquest.com/docview/3003409632/abstract/embedded/7BTGNMKEMPT1V9Z2?source=fedsrch 
856 4 0 |3 Full Text + Graphics  |u https://www.proquest.com/docview/3003409632/fulltextwithgraphics/embedded/7BTGNMKEMPT1V9Z2?source=fedsrch 
856 4 0 |3 Full Text - PDF  |u https://www.proquest.com/docview/3003409632/fulltextPDF/embedded/7BTGNMKEMPT1V9Z2?source=fedsrch