78 research outputs found

    Simulation of Urban Heat Island during a High-Heat Event Using WRF Urban Canopy Models: A Case Study for Metro Manila

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    This present study aims to determine the performance of using the Weather Research and Forecasting (WRF) Model, coupled with the urban canopy models (UCMs), in simulating the 2 m air temperature and 2 m relative humidity in Metro Manila. The simulation was performed during a high heat event on 22–29 April 2018, which coincided with the dry season in the Philippines. The four urban canopy model options that were used in this study include, the bulk (no urban), SLUCM, BEP, and BEM. The results of the simulations were compared with the hourly observations from three weather stations over Metro Manila from the National Oceanic and Atmospheric Administration Integrated Surface Dataset (ISD) and one agrometeorological station in Naic, Cavite. After model validation, the urban heat island (UHI) was then characterized to determine the spatial-temporal variations in the cities of Metro Manila. Statistical results show that the WRF simulation for 2 m air temperature agrees with measurements with an RMSE of0.80. WRF simulation for relative humidity still presents a challenge where simulation errors are higher than the acceptable range. The addition of UCMs does not necessarily improve the simulation for 2 m air temperature, while the use of BEP improved the 2 m relative humidity simulation. The results suggest the importance of using actual urban morphology values in WRF to accurately simulate near-surface variables. On the other hand, WRF simulation shows the presence of urban heat islands, notably in the northwest and central area of Metro Manila during daytime, extending throughout Metro Manila during nighttime. Lower air temperature was consistently observed in areas near Laguna Lake, while higher air temperature due to stagnant winds was observed in the northwest area of Metro Manila. High heat index was also observed throughout Metro Manila from daytime until nighttime, especially in areas near bodies of water like Manila Bay and Laguna Lake due to high humidity

    Nighttime Lights as a Proxy for Economic Performance of Regions

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    Studying and managing regional economic development in the current globalization era demands prompt, reliable, and comparable estimates for a region’s economic performance. Night-time lights (NTL) emitted from residential areas, entertainment places, industrial facilities, etc., and captured by satellites have become an increasingly recognized proxy for on-ground human activities. Compared to traditional indicators supplied by statistical offices, NTLs may have several advantages. First, NTL data are available all over the world, providing researchers and official bodies with the opportunity to obtain estimates even for regions with extremely poor reporting practices. Second, in contrast to non-standardized traditional reporting procedures, the unified NTL data remove the problem of inter-regional comparability. Finally, NTL data are currently globally available on a daily basis, which makes it possible to obtain these estimates promptly. In this book, we provide the reader with the contributions demonstrating the potential and efficiency of using NTL data as a proxy for the performance of regions

    Remote Sensing Monitoring of Land Surface Temperature (LST)

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    This book is a collection of recent developments, methodologies, calibration and validation techniques, and applications of thermal remote sensing data and derived products from UAV-based, aerial, and satellite remote sensing. A set of 15 papers written by a total of 70 authors was selected for this book. The published papers cover a wide range of topics, which can be classified in five groups: algorithms, calibration and validation techniques, improvements in long-term consistency in satellite LST, downscaling of LST, and LST applications and land surface emissivity research

    Vegetation greening offsets urbanization induced fast warming in Guangdong, Hong Kong, and Macao region (GHMR)

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    Previous studies show that the environment in the Guangdong, Hong Kong, and Macao region is under the double stress of global warming and urbanization. Here, we show that due to the increase of regional greenness, the effect of urbanization warming on surface air temperature (SAT) decreased with time and became statistically insignificant from 2004 to 2018, compared to 1979 onward; while the urbanization itself has significantly warmed land surface temperature (LST), with a warming rate of 0.14Β°CΒ Β±Β 0.04Β°C/10a at daytime and 0.02Β°CΒ Β±Β 0.02Β°C/10a at nighttime during 2004–2018, respectively. The anthropogenic heat was found to have a limited influence on SAT, but more significant and tangible effects on LST. It is essential to improve the control of additional warming effects caused by urbanization

    Multisource Remote Sensing based Impervious Surface Mapping

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    Impervious surface (IS) not only serves as a key indicator of urbanization, but also affects the micro-ecosystem. Therefore, it is essential to monitor IS distribution timely and accurately. Remote sensing is an effective approach as it can provide straightforward and consistent information over large area with low cost. This thesis integrates multi-source remote sensing data to interpretate urban patterns and provide more reliable IS mapping results. Registration of optical daytime and nighttime lights (NTL) data is developed in the first contribution. An impervious surface based optical-to-NTL image registration algorithm with iterative blooming effect reduction (IS_iBER) algorithm is proposed. This coarse-to-fine procedure investigates the correlation between optical and NTL features. The iterative registration and blooming effect reduction method obtains precise matching results and reduce the spatial extension of NTL. Considering the spatial transitional nature of urban-rural fringes (URF) areas, the second study proposed approach for URF delineation, namely optical and nighttime lights (NTL) data based multi-scale URF (msON_URF).The landscape heterogeneity and development vitality derived from optical and NTL features are analyzed at a series of scales to illustrate the urban-URF-rural pattern. Results illustrate that msON_URF is effective and practical for not only concentric, but also polycentric urban patterns. The third study proposes a nighttime light adjusted impervious surface index (NAISI) to detect IS area. Parallel to baseline subtraction approaches, NAISI takes advantage of features, rather than spectral band information to map IS. NAISI makes the most of independence between NTL-ISS and pervious surface to address the high spectral similarity between IS and bare soil in optical image. An optical and NTL based spectral mixture analysis (ON_SMA) is proposed to achieve sub-pixel IS mapping result in the fourth study. It integrates characteristics of optical and NTL imagery to adaptively select local endmembers. Results illustrate the proposed method yields effective improvement and highlight the potential of NTL data in IS mapping. In the fifth study, GA-SVM IS mapping algorithm is investigated with introduction of the achieved urban-URF-rural spatial structure. The combination of optical, NTL and SAR imagery is discussed. GA is implemented for feature selection and parameter optimization in each urban scenario

    Land surface temperature and evapotranspiration estimation in the Amazon evergreen forests using remote sensing data

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    Amazonian tropical forests play a significant role in global water, carbon and energy cycles. Considering the relevance of this biome and the climate change projections which predict a hotter and drier climate for the region, the monitoring of the vegetation status of these forests becomes of significant importance. In this context, vegetation temperature and evapotranspiration (ET) can be considered as key variables. Vegetation temperature is directly linked with plant physiology. In addition, some studies have shown the existing relationship between this variable and the CO2 absorption capacity and biomass loss of these forests. Evapotranspiration resulting from the combined processes of transpiration and evaporation links the terrestrial water, carbon and surface energy exchanges of these forests. How this variable will response to the changing climate is critical to understand the stability of these forests. Satellite remote sensing is presented as a feasible means in order to provide accurate spatially-distributed estimates of these variables. Nevertheless, the use of satellite passive imagery for analysing this region still has some limitations being of special importance the proper cloud masking of the satellite data which becomes a difficult task due to the continuous cloud cover of the region. Under the light of the aforementioned issues, the present doctoral thesis is aimed at estimating the land surface temperature and evapotranspiration of the Amazonian tropical forests using remote sensing data. In addition, as cloud screening of satellite imagery is a critical step in the processing chain of the previous magnitudes and becomes of special importance for the study region this topic has also been included in this thesis. We have mainly focused on the use of data from the Moderate Resolution Imaging Spectroradiometer (MODIS) which is amongst major tools for studying this region. Regarding the cloud detection topic, the potential of supervised learning algorithms for cloud masking was studied in order to overcome the cloud contamination issue of the current satellite products. Models considered were: Gaussian NaΓ―ve Bayes (GNB), Linear Discriminant Analysis (LDA), Quadratic Discriminant Analysis (QDA), Random Forests (RF), Support Vector Machine (SVM) and Multilayer Perceptron (MLP). These algorithms are able to provide a continuous measure of cloud masking uncertainty (i.e. a probability estimate of each pixel belonging to clear and cloudy class) and therefore can be used under the light of a probabilistic approach. Reference dataset (a priori knowledge) requirement was satisfied by considering the collocation of Cloud Profiling Radar (CPR) and Cloud Aerosol Lidar with Orthogonal Polarization (CALIOP) observations with MODIS sensor. Model performance was tested using three independent datasets: 1) collocated CPR/CALIOP and MODIS data, 2) MODIS manually classified images and 3) in-situ ground data. For the case of satellite image and in-situ testing, results were additionally compared to current operative MYD35 (version 6.1) and Multi-Angle Implementation of the Atmospheric Correction (MAIAC) cloud masking algorithms. These results showed that machine learning algorithms were able to improve MODIS operative cloud masking performance over the region. MYD35 and MAIAC tended to underestimate and overestimate the cloud cover, respectively. Amongst the models considered, LDA stood out as the best candidate because of its maximum accuracy (difference in Kappa coefficient of 0.293/0.155 (MYD35 /MAIAC respectively)) and minimum computational associated. Regarding the estimation of land surface temperature (LST), the aim of this study was to generate specific LST products for the Amazonian tropical forests. This goal was accomplished by using a tuned split-window (SW) equation. Validation of the LST products was obtained by direct comparison between LST estimates as derived from the algorithms and two types of different LST observations: in-situ LST (T-based validation) and LST derived from the R-based method. In addition, LST algorithms were validated using independent simulated data. In-situ LST was retrieved from two infrared radiometers (SI-100 and IR-120) and a CNR4 net radiometer, situated at Tambopata test site (12.832 S, 62.282 W) in the Peruvian Amazon. Apart from this, current satellite LST products were also validated and compared to the tuned split-window. Although we have mainly focus on MODIS LST products which derive from three different LST algorithms: split-window, day and night (DN) and Temperature Emissivity Separation (TES), we have also considered the inclusion of the Visible Infrared Imaging Radiometer Suite (VIIRS) sensor. In addition, a first assessment of the Sea and Land Surface Temperature Radiometer (SLSTR) is presented. Validation was performed separately for daytime and nighttime conditions. For MODIS sensor, current LST products showed Root Mean Square Errors (RMSE) in LST estimations between 2 K and 3K for daytime and 1 K and 2 K for nighttime. In the best case (with a restrictive cloud screening) RMSE errors decrease to values below 2K and around 1 K, respectively. The proposed LST showed RMSE values of 1K to approximately 2 K and 0.7-1.5 K (below 1.5 K and below 1 K in the best case) for daytime and nighttime conditions, thus improving current LST MODIS products. This is also in agreement with the R-based validation results, which show a RMSE reduction of 0.7 K to 1.7 K in comparison to MODIS LST products. For the case of VIIRS sensor daytime conditions, VIIRS-TES algorithm provides the best performance with a difference of 0.2 K to around 0.3 K in RMSE regarding the split window algorithm (in the best case it reduces to 0.2 K). All VIIRS LST products considered have RMSE values between 2 K and 3K. At nighttime, however VIIRS-TES is not able to outperform the SW algorithm. A difference of 0.7 K to 0.8 K in RMSE is obtained. Contrary to MODIS and the SW LST products, VIIRS-TES tends to overestimate in-situ LST values. Regarding SLSTR sensor, the L2 product provides a better agreement with in-situ observations than the proposed algorithm (daytime difference in RMSE around 0.6 K and up 0.07 K at nighttime). In the estimation of the ET, we focused on the evaluation of four commonly used remote-sensing based ET models. These were: i) Priestley-Taylor Jet Propulsion Laboratory (PT-JPL), ii) Penman-Monteith MODIS operative parametrization (PM-Mu), iii) Surface Energy Balance System (SEBS), and iv) Satellite Application Facility on Land Surface Analysis (LSASAF). These models were forced using remote-sensing data from MODIS and two ancillary meteorological data sources: i) in-situ data extracted from Large-Scale Biosphere-Atmosphere Experiment (LBA) stations (scenario I), and ii) three reanalysis datasets (scenario II), including Modern-Era Retrospective analysis for Research and Application (MERRA-2), European Centre for Medium-range Weather Forecasts (ECMWF) Re-Analysis-Interim (ERA-Interim), and Global Land Assimilation System (GLDAS-2.1). Performance of algorithms under the two scenarios was validated using in-situ eddy-covariance measurements. For scenario I, PT-JPL provided the best agreement with in-situ ET observations (RMSE = 0.55 mm/day, R = 0.88). Neglecting water canopy evaporation resulted in an underestimation of ET measurements for LSASAF. SEBS performance was similar to that of PT-JPL, nevertheless SEBS estimates were limited by the continuous cloud cover of the region. A physically-based ET gap-filling method was used in order to alleviate this issue. PM-Mu also with a similar performance to PT-JPL tended to overestimate in-situ ET observations. For scenario II, quality assessment of reanalysis input data demonstrated that MERRA-2, ERA-Interim and GLDAS-2.1 contain biases that impact model performance. In particular, biases in radiation inputs were found the main responsible of the observed biases in ET estimates. For the region, MERRA-2 tends to overestimate daily net radiation and incoming solar radiation. ERA-Interim tends to underestimate both variables, and GLDAS-2.1 tends to overestimate daily radiation while underestimating incoming solar radiation. Discrepancies amongst these inputs resulted in large absolute deviations in spatial patterns (deviations greater than 500 mm/year) and temporal patterns

    Remote sensing of night lights: a review and an outlook for the future

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    This is the author accepted manuscript. The final version is available from Elsevier via the DOI in this recordRemote sensing of night light emissions in the visible band offers a unique opportunity to directly observe human activity from space. This has allowed a host of applications including mapping urban areas, estimating population and GDP, monitoring disasters and conflicts. More recently, remotely sensed night lights data have found use in understanding the environmental impacts of light emissions (light pollution), including their impacts on human health. In this review, we outline the historical development of night-time optical sensors up to the current state of the art sensors, highlight various applications of night light data, discuss the special challenges associated with remote sensing of night lights with a focus on the limitations of current sensors, and provide an outlook for the future of remote sensing of night lights. While the paper mainly focuses on space borne remote sensing, ground based sensing of night-time brightness for studies on astronomical and ecological light pollution, as well as for calibration and validation of space borne data, are also discussed. Although the development of night light sensors lags behind day-time sensors, we demonstrate that the field is in a stage of rapid development. The worldwide transition to LED lights poses a particular challenge for remote sensing of night lights, and strongly highlights the need for a new generation of space borne night lights instruments. This work shows that future sensors are needed to monitor temporal changes during the night (for example from a geostationary platform or constellation of satellites), and to better understand the angular patterns of light emission (roughly analogous to the BRDF in daylight sensing). Perhaps most importantly, we make the case that higher spatial resolution and multispectral sensors covering the range from blue to NIR are needed to more effectively identify lighting technologies, map urban functions, and monitor energy use.European Union Horizon 2020Helmholtz AssociationNatural Environment Research Council (NERC)Chinese Academy of ScienceLeibniz AssociationIGB Leibniz Institut

    Responses of Land Surface Phenology to Wildfire Disturbances in the Western United States Forests

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    Land surface phenology (LSP) characterizes the seasonal dynamics in the vegetation communities observed for a satellite pixel and it has been widely associated with global climate change. However, LSP and its long-term trend can be influenced by land disturbance events, which could greatly interrupt the LSP responses to climate change. Wildfire is one of the main disturbance agents in the western United States (US) forests, but its impacts on LSP have not been investigated yet. To gain a comprehensive understanding of the LSP responses to wildfires in the western US forests, this dissertation focused on three research objectives: (1) to perform a case study of wildfire impacts on LSP and its trend by comparing the burned and a reference area, (2) to investigate the distribution of wildfire impacts on LSP and identify control factors by analyzing all the wildfires across the western US forests, and (3) to quantify the contributions of land cover composition and other environmental factors to the spatial and interannual variations of LSP in a recently burned landscape. The results reveal that wildfires play a significant role in influencing spatial and interannual variations in LSP across the western US forests. First, the case study showed that the Hayman Fire significantly advanced the start of growing season (SOS) and caused an advancing SOS trend comparing with a delaying trend in the reference area. Second, summarizing \u3e800 wildfires found that the shifts in LSP timing were divergent depending on individual wildfire events and burn severity. Moreover, wildfires showed a stronger impact on the end of growing season (EOS) than SOS. Last, LSP trends were interrupted by wildfires with the degree of impact largely dependent on the wildfire occurrence year. Third, LSP modeling showed that land cover composition, climate, and topography co-determine the LSP variations. Specifically, land cover composition and climate dominate the LSP spatial and interannual variations, respectively. Overall, this research improves the understanding of wildfire impacts on LSP and the underlying mechanism of various factors driving LSP. This research also provides a prototype that can be extended to investigate the impacts on LSP from other disturbances

    μ‹œκ³΅κ°„ 해상도 ν–₯상을 ν†΅ν•œ 식생 λ³€ν™” λͺ¨λ‹ˆν„°λ§

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    ν•™μœ„λ…Όλ¬Έ(박사) -- μ„œμšΈλŒ€ν•™κ΅λŒ€ν•™μ› : ν™˜κ²½λŒ€ν•™μ› ν˜‘λ™κ³Όμ • μ‘°κ²½ν•™, 2023. 2. λ₯˜μ˜λ ¬.μœ‘μƒ μƒνƒœκ³„μ—μ„œ λŒ€κΈ°κΆŒκ³Ό μƒλ¬ΌκΆŒμ˜ μƒν˜Έ μž‘μš©μ„ μ΄ν•΄ν•˜κΈ° μœ„ν•΄μ„œλŠ” 식생 λ³€ν™”μ˜ λͺ¨λ‹ˆν„°λ§μ΄ ν•„μš”ν•˜λ‹€. 이 λ•Œ, μœ„μ„±μ˜μƒμ€ μ§€ν‘œλ©΄μ„ κ΄€μΈ‘ν•˜μ—¬ 식생지도λ₯Ό μ œκ³΅ν•  수 μžˆμ§€λ§Œ, μ§€ν‘œλ³€ν™”μ˜ μƒμ„Έν•œ μ •λ³΄λŠ” κ΅¬λ¦„μ΄λ‚˜ μœ„μ„± μ΄λ―Έμ§€μ˜ 곡간 해상도에 μ˜ν•΄ μ œν•œλ˜μ—ˆλ‹€. λ˜ν•œ μœ„μ„±μ˜μƒμ˜ μ‹œκ³΅κ°„ 해상도가 식생지도λ₯Ό ν†΅ν•œ κ΄‘ν•©μ„± λͺ¨λ‹ˆν„°λ§μ— λ―ΈμΉ˜λŠ” 영ν–₯은 μ™„μ „νžˆ λ°ν˜€μ§€μ§€ μ•Šμ•˜λ‹€. λ³Έ λ…Όλ¬Έμ—μ„œλŠ” 고해상도 식생 지도λ₯Ό μΌλ‹¨μœ„λ‘œ μƒμ„±ν•˜κΈ° μœ„μ„± μ˜μƒμ˜ μ‹œκ³΅κ°„ 해상도λ₯Ό ν–₯μƒμ‹œν‚€λŠ” 것을 λͺ©ν‘œλ‘œ ν•˜μ˜€λ‹€. 고해상도 μœ„μ„±μ˜μƒμ„ ν™œμš©ν•œ 식생 λ³€ν™” λͺ¨λ‹ˆν„°λ§μ„ μ‹œκ³΅κ°„μ μœΌλ‘œ ν™•μž₯ν•˜κΈ° μœ„ν•΄ 1) 정지ꢀ도 μœ„μ„±μ„ ν™œμš©ν•œ μ˜μƒμœ΅ν•©μ„ 톡해 μ‹œκ°„ν•΄μƒλ„ ν–₯상, 2) μ λŒ€μ μƒμ„±λ„€νŠΈμ›Œν¬λ₯Ό ν™œμš©ν•œ 곡간해상도 ν–₯상, 3) μ‹œκ³΅κ°„ν•΄μƒλ„κ°€ 높은 μœ„μ„±μ˜μƒμ„ 토지피볡이 κ· μ§ˆν•˜μ§€ μ•Šμ€ κ³΅κ°„μ—μ„œ 식물 κ΄‘ν•©μ„± λͺ¨λ‹ˆν„°λ§μ„ μˆ˜ν–‰ν•˜μ˜€λ‹€. 이처럼, μœ„μ„±κΈ°λ°˜ μ›κ²©νƒμ§€μ—μ„œ μƒˆλ‘œμš΄ 기술이 λ“±μž₯함에 따라 ν˜„μž¬ 및 과거의 μœ„μ„±μ˜μƒμ€ μ‹œκ³΅κ°„ 해상도 μΈ‘λ©΄μ—μ„œ ν–₯μƒλ˜μ–΄ 식생 λ³€ν™”μ˜ λͺ¨λ‹ˆν„°λ§ ν•  수 μžˆλ‹€. 제2μž₯μ—μ„œλŠ” μ •μ§€κΆ€λ„μœ„μ„±μ˜μƒμ„ ν™œμš©ν•˜λŠ” μ‹œκ³΅κ°„ μ˜μƒμœ΅ν•©μœΌλ‘œ μ‹λ¬Όμ˜ 광합성을 λͺ¨λ‹ˆν„°λ§ ν–ˆμ„ λ•Œ, μ‹œκ°„ν•΄μƒλ„κ°€ ν–₯상됨을 λ³΄μ˜€λ‹€. μ‹œκ³΅κ°„ μ˜μƒμœ΅ν•© μ‹œ, ꡬ름탐지, μ–‘λ°©ν–₯ λ°˜μ‚¬ ν•¨μˆ˜ μ‘°μ •, 곡간 등둝, μ‹œκ³΅κ°„ μœ΅ν•©, μ‹œκ³΅κ°„ 결츑치 보완 λ“±μ˜ 과정을 κ±°μΉœλ‹€. 이 μ˜μƒμœ΅ν•© μ‚°μΆœλ¬Όμ€ κ²½μž‘κ΄€λ¦¬ λ“±μœΌλ‘œ 식생 μ§€μˆ˜μ˜ μ—°κ°„ 변동이 큰 두 μž₯μ†Œ(농경지와 λ‚™μ—½μˆ˜λ¦Ό)μ—μ„œ ν‰κ°€ν•˜μ˜€λ‹€. κ·Έ κ²°κ³Ό, μ‹œκ³΅κ°„ μ˜μƒμœ΅ν•© μ‚°μΆœλ¬Όμ€ 결츑치 없이 ν˜„μž₯관츑을 μ˜ˆμΈ‘ν•˜μ˜€λ‹€ (R2 = 0.71, μƒλŒ€ 편ν–₯ = 5.64% 농경지; R2 = 0.79, μƒλŒ€ 편ν–₯ = -13.8%, ν™œμ—½μˆ˜λ¦Ό). μ‹œκ³΅κ°„ μ˜μƒμœ΅ν•©μ€ 식생 μ§€λ„μ˜ μ‹œκ³΅κ°„ 해상도λ₯Ό μ μ§„μ μœΌλ‘œ κ°œμ„ ν•˜μ—¬, 식물 생μž₯κΈ°λ™μ•ˆ μœ„μ„±μ˜μƒμ΄ ν˜„μž₯ 관츑을 κ³Όμ†Œ 평가λ₯Ό μ€„μ˜€λ‹€. μ˜μƒμœ΅ν•©μ€ 높은 μ‹œκ³΅κ°„ ν•΄μƒλ„λ‘œ κ΄‘ν•©μ„± 지도λ₯Ό μΌκ°„κ²©μœΌλ‘œ μƒμ„±ν•˜κΈ°μ— 이λ₯Ό ν™œμš©ν•˜μ—¬ μœ„μ„± μ˜μƒμ˜ μ œν•œλœ μ‹œκ³΅κ°„ ν•΄μƒλ„λ‘œ λ°ν˜€μ§€μ§€ μ•Šμ€ μ‹λ¬Όλ³€ν™”μ˜ 과정을 λ°œκ²¬ν•˜κΈΈ κΈ°λŒ€ν•œλ‹€. μ‹μƒμ˜ 곡간뢄포은 정밀농업과 토지 피볡 λ³€ν™” λͺ¨λ‹ˆν„°λ§μ„ μœ„ν•΄ ν•„μˆ˜μ μ΄λ‹€. 고해상도 μœ„μ„±μ˜μƒμœΌλ‘œ 지ꡬ ν‘œλ©΄μ„ κ΄€μΈ‘ν•˜λŠ” 것을 μš©μ΄ν•˜κ²Œ ν•΄μ‘Œλ‹€. 특히 Planet Fusion은 μ΄ˆμ†Œν˜•μœ„μ„±κ΅° 데이터λ₯Ό μ΅œλŒ€ν•œ ν™œμš©ν•΄ 데이터 결츑이 μ—†λŠ” 3m 곡간 ν•΄μƒλ„μ˜ μ§€ν‘œ ν‘œλ©΄ λ°˜μ‚¬λ„μ΄λ‹€. κ·ΈλŸ¬λ‚˜ κ³Όκ±° μœ„μ„± μ„Όμ„œ(Landsat의 경우 30~60m)의 곡간 ν•΄μƒλ„λŠ” μ‹μƒμ˜ 곡간적 λ³€ν™”λ₯Ό 상세 λΆ„μ„ν•˜λŠ” 것을 μ œν•œν–ˆλ‹€. 제3μž₯μ—μ„œλŠ” Landsat λ°μ΄ν„°μ˜ 곡간 해상도λ₯Ό ν–₯μƒν•˜κΈ° μœ„ν•΄ Planet Fusion 및 Landsat 8 데이터λ₯Ό μ‚¬μš©ν•˜μ—¬ 이쀑 μ λŒ€μ  생성 λ„€νŠΈμ›Œν¬(the dual RSS-GAN)λ₯Ό ν•™μŠ΅μ‹œμΌœ, 고해상도 μ •κ·œν™” 식생 μ§€μˆ˜(NDVI)와 식물 근적외선 λ°˜μ‚¬(NIRv)도λ₯Ό μƒμ„±ν•˜λŠ” ν•œλ‹€. νƒ€μ›ŒκΈ°λ°˜ ν˜„μž₯ μ‹μƒμ§€μˆ˜(μ΅œλŒ€ 8λ…„)와 λ“œλ‘ κΈ°λ°˜ μ΄ˆλΆ„κ΄‘μ§€λ„λ‘œ the dual RSS-GAN의 μ„±λŠ₯을 λŒ€ν•œλ―Όκ΅­ λ‚΄ 두 λŒ€μƒμ§€(농경지와 ν™œμ—½μˆ˜λ¦Ό)μ—μ„œ ν‰κ°€ν–ˆλ‹€. The dual RSS-GAN은 Landsat 8 μ˜μƒμ˜ 곡간해상도λ₯Ό ν–₯μƒμ‹œμΌœ 곡간 ν‘œν˜„μ„ λ³΄μ™„ν•˜κ³  식생 μ§€μˆ˜μ˜ κ³„μ ˆμ  λ³€ν™”λ₯Ό ν¬μ°©ν–ˆλ‹€(R2> 0.96). 그리고 the dual RSS-GAN은 Landsat 8 식생 μ§€μˆ˜κ°€ ν˜„μž₯에 λΉ„ν•΄ κ³Όμ†Œ ν‰κ°€λ˜λŠ” 것을 μ™„ν™”ν–ˆλ‹€. ν˜„μž₯ 관츑에 λΉ„ν•΄ 이쀑 RSS-GANκ³Ό Landsat 8의 μƒλŒ€ 편ν–₯ κ°’ 각각 -0.8% μ—μ„œ -1.5%, -10.3% μ—μ„œ -4.6% μ˜€λ‹€. μ΄λŸ¬ν•œ κ°œμ„ μ€ Planet Fusion의 곡간정보λ₯Ό 이쀑 RSS-GAN둜 ν•™μŠ΅ν•˜μ˜€κΈ°μ— κ°€λŠ₯ν–ˆλ‹€. ν—€λ‹Ή 연ꡬ κ²°κ³ΌλŠ” Landsat μ˜μƒμ˜ 곡간 해상도λ₯Ό ν–₯μƒμ‹œμΌœ μˆ¨κ²¨μ§„ 곡간 정보λ₯Ό μ œκ³΅ν•˜λŠ” μƒˆλ‘œμš΄ μ ‘κ·Ό 방식이닀. κ³ ν•΄μƒλ„μ—μ„œ 식물 κ΄‘ν•©μ„± μ§€λ„λŠ” 토지피볡이 λ³΅μž‘ν•œ κ³΅κ°„μ—μ„œ νƒ„μ†Œ μˆœν™˜ λͺ¨λ‹ˆν„°λ§μ‹œ ν•„μˆ˜μ μ΄λ‹€. κ·ΈλŸ¬λ‚˜ Sentinel-2, Landsat 및 MODIS와 같이 νƒœμ–‘ 동쑰 ꢀ도에 μžˆλŠ” μœ„μ„±μ€ 곡간 해상도가 λ†’κ±°λ‚˜ μ‹œκ°„ 해상도 높은 μœ„μ„±μ˜μƒλ§Œ μ œκ³΅ν•  수 μžˆλ‹€. 졜근 λ°œμ‚¬λœ μ΄ˆμ†Œν˜•μœ„μ„±κ΅°μ€ μ΄λŸ¬ν•œ 해상도 ν•œκ³„μ„ 극볡할 수 μžˆλ‹€. 특히 Planet Fusion은 μ΄ˆμ†Œν˜•μœ„μ„± 자료의 μ‹œκ³΅κ°„ ν•΄μƒλ„λ‘œ μ§€ν‘œλ©΄μ„ κ΄€μΈ‘ν•  수 μžˆλ‹€. 4μž₯μ—μ„œ, Planet Fusion μ§€ν‘œλ°˜μ‚¬λ„λ₯Ό μ΄μš©ν•˜μ—¬ μ‹μƒμ—μ„œ λ°˜μ‚¬λœ 근적외선 볡사(NIRvP)λ₯Ό 3m 해상도 지도λ₯Ό μΌκ°„κ²©μœΌλ‘œ μƒμ„±ν–ˆλ‹€. 그런 λ‹€μŒ λ―Έκ΅­ μΊ˜λ¦¬ν¬λ‹ˆμ•„μ£Ό μƒˆν¬λΌλ©˜ν† -μƒŒ ν˜Έμ•„ν‚¨ λΈνƒ€μ˜ ν”ŒλŸ­μŠ€ νƒ€μ›Œ λ„€νŠΈμ›Œν¬ 데이터와 λΉ„κ΅ν•˜μ—¬ 식물 광합성을 μΆ”μ •ν•˜κΈ° μœ„ν•œ NIRvP μ§€λ„μ˜ μ„±λŠ₯을 ν‰κ°€ν•˜μ˜€λ‹€. μ „μ²΄μ μœΌλ‘œ NIRvP μ§€λ„λŠ” μŠ΅μ§€μ˜ μž¦μ€ μˆ˜μœ„ 변화에도 λΆˆκ΅¬ν•˜κ³  κ°œλ³„ λŒ€μƒμ§€μ˜ 식물 κ΄‘ν•©μ„±μ˜ μ‹œκ°„μ  λ³€ν™”λ₯Ό ν¬μ°©ν•˜μ˜€λ‹€. κ·ΈλŸ¬λ‚˜ λŒ€μƒμ§€ 전체에 λŒ€ν•œ NIRvP 지도와 식물 κ΄‘ν•©μ„± μ‚¬μ΄μ˜ κ΄€κ³„λŠ” NIRvP 지도λ₯Ό ν”ŒλŸ­μŠ€ νƒ€μ›Œ κ΄€μΈ‘λ²”μœ„μ™€ μΌμΉ˜μ‹œν‚¬ λ•Œλ§Œ 높은 상관관계λ₯Ό λ³΄μ˜€λ‹€. κ΄€μΈ‘λ²”μœ„λ₯Ό μΌμΉ˜μ‹œν‚¬ 경우, NIRvP μ§€λ„λŠ” 식물 광합성을 μΆ”μ •ν•˜λŠ” 데 μžˆμ–΄ ν˜„μž₯ NIRvP보닀 μš°μˆ˜ν•œ μ„±λŠ₯을 λ³΄μ˜€λ‹€. μ΄λŸ¬ν•œ μ„±λŠ₯ μ°¨μ΄λŠ” ν”ŒλŸ­μŠ€ νƒ€μ›Œ κ΄€μΈ‘λ²”μœ„λ₯Ό μΌμΉ˜μ‹œν‚¬ λ•Œ, 연ꡬ λŒ€μƒμ§€ κ°„μ˜ NIRvP-식물 κ΄‘ν•©μ„± κ΄€κ³„μ˜ κΈ°μšΈκΈ°κ°€ 일관성을 λ³΄μ˜€κΈ° λ•Œλ¬Έμ΄λ‹€. λ³Έ 연ꡬ κ²°κ³ΌλŠ” μœ„μ„± 관츑을 ν”ŒλŸ­μŠ€ νƒ€μ›Œ κ΄€μΈ‘λ²”μœ„μ™€ μΌμΉ˜μ‹œν‚€λŠ” κ²ƒμ˜ μ€‘μš”μ„±μ„ 보여주고 높은 μ‹œκ³΅κ°„ ν•΄μƒλ„λ‘œ 식물 광합성을 μ›κ²©μœΌλ‘œ λͺ¨λ‹ˆν„°λ§ν•˜λŠ” μ΄ˆμ†Œν˜•μœ„μ„±κ΅° 자료의 잠재λ ₯을 보여쀀닀.Monitoring changes in terrestrial vegetation is essential to understanding interactions between atmosphere and biosphere, especially terrestrial ecosystem. To this end, satellite remote sensing offer maps for examining land surface in different scales. However, the detailed information was hindered under the clouds or limited by the spatial resolution of satellite imagery. Moreover, the impacts of spatial and temporal resolution in photosynthesis monitoring were not fully revealed. In this dissertation, I aimed to enhance the spatial and temporal resolution of satellite imagery towards daily gap-free vegetation maps with high spatial resolution. In order to expand vegetation change monitoring in time and space using high-resolution satellite images, I 1) improved temporal resolution of satellite dataset through image fusion using geostationary satellites, 2) improved spatial resolution of satellite dataset using generative adversarial networks, and 3) showed the use of high spatiotemporal resolution maps for monitoring plant photosynthesis especially over heterogeneous landscapes. With the advent of new techniques in satellite remote sensing, current and past datasets can be fully utilized for monitoring vegetation changes in the respect of spatial and temporal resolution. In Chapter 2, I developed the integrated system that implemented geostationary satellite products in the spatiotemporal image fusion method for monitoring canopy photosynthesis. The integrated system contains the series of process (i.e., cloud masking, nadir bidirectional reflectance function adjustment, spatial registration, spatiotemporal image fusion, spatial gap-filling, temporal-gap-filling). I conducted the evaluation of the integrated system over heterogeneous rice paddy landscape where the drastic land cover changes were caused by cultivation management and deciduous forest where consecutive changes occurred in time. The results showed that the integrated system well predict in situ measurements without data gaps (R2 = 0.71, relative bias = 5.64% at rice paddy site; R2 = 0.79, relative bias = -13.8% at deciduous forest site). The integrated system gradually improved the spatiotemporal resolution of vegetation maps, reducing the underestimation of in situ measurements, especially during peak growing season. Since the integrated system generates daily canopy photosynthesis maps for monitoring dynamics among regions of interest worldwide with high spatial resolution. I anticipate future efforts to reveal the hindered information by the limited spatial and temporal resolution of satellite imagery. Detailed spatial representations of terrestrial vegetation are essential for precision agricultural applications and the monitoring of land cover changes in heterogeneous landscapes. The advent of satellite-based remote sensing has facilitated daily observations of the Earths surface with high spatial resolution. In particular, a data fusion product such as Planet Fusion has realized the delivery of daily, gap-free surface reflectance data with 3-m pixel resolution through full utilization of relatively recent (i.e., 2018-) CubeSat constellation data. However, the spatial resolution of past satellite sensors (i.e., 30–60 m for Landsat) has restricted the detailed spatial analysis of past changes in vegetation. In Chapter 3, to overcome the spatial resolution constraint of Landsat data for long-term vegetation monitoring, we propose a dual remote-sensing super-resolution generative adversarial network (dual RSS-GAN) combining Planet Fusion and Landsat 8 data to simulate spatially enhanced long-term time-series of the normalized difference vegetation index (NDVI) and near-infrared reflectance from vegetation (NIRv). We evaluated the performance of the dual RSS-GAN against in situ tower-based continuous measurements (up to 8 years) and remotely piloted aerial system-based maps of cropland and deciduous forest in the Republic of Korea. The dual RSS-GAN enhanced spatial representations in Landsat 8 images and captured seasonal variation in vegetation indices (R2 > 0.95, for the dual RSS-GAN maps vs. in situ data from all sites). Overall, the dual RSS-GAN reduced Landsat 8 vegetation index underestimations compared with in situ measurements; relative bias values of NDVI ranged from βˆ’3.2% to 1.2% and βˆ’12.4% to βˆ’3.7% for the dual RSS-GAN and Landsat 8, respectively. This improvement was caused by spatial enhancement through the dual RSS-GAN, which captured fine-scale information from Planet Fusion. This study presents a new approach for the restoration of hidden sub-pixel spatial information in Landsat images. Mapping canopy photosynthesis in both high spatial and temporal resolution is essential for carbon cycle monitoring in heterogeneous areas. However, well established satellites in sun-synchronous orbits such as Sentinel-2, Landsat and MODIS can only provide either high spatial or high temporal resolution but not both. Recently established CubeSat satellite constellations have created an opportunity to overcome this resolution trade-off. In particular, Planet Fusion allows full utilization of the CubeSat data resolution and coverage while maintaining high radiometric quality. In Chapter 4, I used the Planet Fusion surface reflectance product to calculate daily, 3-m resolution, gap-free maps of the near-infrared radiation reflected from vegetation (NIRvP). I then evaluated the performance of these NIRvP maps for estimating canopy photosynthesis by comparing with data from a flux tower network in Sacramento-San Joaquin Delta, California, USA. Overall, NIRvP maps captured temporal variations in canopy photosynthesis of individual sites, despite changes in water extent in the wetlands and frequent mowing in the crop fields. When combining data from all sites, however, I found that robust agreement between NIRvP maps and canopy photosynthesis could only be achieved when matching NIRvP maps to the flux tower footprints. In this case of matched footprints, NIRvP maps showed considerably better performance than in situ NIRvP in estimating canopy photosynthesis both for daily sum and data around the time of satellite overpass (R2 = 0.78 vs. 0.60, for maps vs. in situ for the satellite overpass time case). This difference in performance was mostly due to the higher degree of consistency in slopes of NIRvP-canopy photosynthesis relationships across the study sites for flux tower footprint-matched maps. Our results show the importance of matching satellite observations to the flux tower footprint and demonstrate the potential of CubeSat constellation imagery to monitor canopy photosynthesis remotely at high spatio-temporal resolution.Chapter 1. Introduction 2 1. Background 2 1.1 Daily gap-free surface reflectance using geostationary satellite products 2 1.2 Monitoring past vegetation changes with high-spatial-resolution 3 1.3 High spatiotemporal resolution vegetation photosynthesis maps 4 2. Purpose of Research 4 Chapter 2. Generating daily gap-filled BRDF adjusted surface reflectance product at 10 m resolution using geostationary satellite product for monitoring daily canopy photosynthesis 6 1. Introduction 6 2. Methods 11 2.1 Study sites 11 2.2 In situ measurements 13 2.3 Satellite products 14 2.4 Integrated system 17 2.5 Canopy photosynthesis 21 2.6 Evaluation 23 3. Results and discussion 24 3.1 Comparison of STIF NDVI and NIRv with in situ NDVI and NIRv 24 3.2 Comparison of STIF NIRvP with in situ NIRvP 28 4. Conclusion 31 Chapter 3. Super-resolution of historic Landsat imagery using a dual Generative Adversarial Network (GAN) model with CubeSat constellation imagery for monitoring vegetation changes 32 1. Introduction 32 2. Methods 38 2.1 Real-ESRGAN model 38 2.2 Study sites 40 2.3 In situ measurements 42 2.4 Vegetation index 44 2.5 Satellite data 45 2.6 Planet Fusion 48 2.7 Dual RSS-GAN via fine-tuned Real-ESRGAN 49 2.8 Evaluation 54 3. Results 57 3.1 Comparison of NDVI and NIRv maps from Planet Fusion, Sentinel 2 NBAR, and Landsat 8 NBAR data with in situ NDVI and NIRv 57 3.2 Comparison of dual RSS-SRGAN model results with Landsat 8 NDVI and NIRv 60 3.3 Comparison of dual RSS-GAN model results with respect to in situ time-series NDVI and NIRv 63 3.4 Comparison of the dual RSS-GAN model with NDVI and NIRv maps derived from RPAS 66 4. Discussion 70 4.1 Monitoring changes in terrestrial vegetation using the dual RSS-GAN model 70 4.2 CubeSat data in the dual RSS-GAN model 72 4.3 Perspectives and limitations 73 5. Conclusion 78 Appendices 79 Supplementary material 82 Chapter 4. Matching high resolution satellite data and flux tower footprints improves their agreement in photosynthesis estimates 85 1. Introduction 85 2. Methods 89 2.1 Study sites 89 2.2 In situ measurements 92 2.3 Planet Fusion NIRvP 94 2.4 Flux footprint model 98 2.5 Evaluation 98 3. Results 105 3.1 Comparison of Planet Fusion NIRv and NIRvP with in situ NIRv and NIRvP 105 3.2 Comparison of instantaneous Planet Fusion NIRv and NIRvP with against tower GPP estimates 108 3.3 Daily GPP estimation from Planet Fusion -derived NIRvP 114 4. Discussion 118 4.1 Flux tower footprint matching and effects of spatial and temporal resolution on GPP estimation 118 4.2 Roles of radiation component in GPP mapping 123 4.3 Limitations and perspectives 126 5. Conclusion 133 Appendix 135 Supplementary Materials 144 Chapter 5. Conclusion 153 Bibliography 155 Abstract in Korea 199 Acknowledgements 202λ°•
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