scholarly journals Characterization of vegetation fraction estimated using spot-vegetation NDVI data for regional climate modeling in India

MAUSAM ◽  
2021 ◽  
Vol 57 (4) ◽  
pp. 669-674
Author(s):  
S. R. OZA ◽  
R. P. SINGH ◽  
V. K. DADHWAL

lkj & ,e- ,e- 5 tSls eslksLdsy tyok;q fun’kksZa }kjk ouLifr ¼oh- ,Q-½ dh lwpuk nsus dk dk;Z egRoiw.kZ gSA fun’kZu ¼ekWMfyax½ esa lkekU; :Ik ls lcls vf/kd iz;qDr dh xbZ tyok;q laca/kh ekfld oh- ,Q-  gSA oh- ,Q- dh lwpuk,¡ ,u- vks- ,- ,- & ,- oh- ,p- vkj- vkj-  ,u- Mh- oh- vkbZ- HkweaMyh; vk¡dM+k lsVksa dk mi;ksx djrs gq, xqVesu vkSj bXukVkso ¼1988½ ¼th- vkbZ-½ }kjk rS;kj dh xbZ gSA bl 'kks/k&i= esa Hkkjrh; {ks= ds vizSy 1998 ls uoacj 2003 dh vof/k ds LikWV& ost+hVs’ku 10 fnolh; fefJr ,u- Mh- oh- vkbZ- ds mRiknksa dk mi;ksx djrs gq, 1 fd- eh- ds oh- ,Q- ds vk¡dM+k lsV rS;kj djus ds ckjs esa crk;k x;k gSA LikWV&osthVs’ku ds 0 % vkSj 100 % dh  oh- ,Q- ls laca) ,u- Mh- oh- vkbZ- dh laosnd fof’k"V izHkkolhek,¡ th- vkbZ- ds 0-04 vkSj 0-52 dh rqyuk esa Øe’k: 0-04 vkSj 0-804 ikbZ xbZaA th- vkbZ- ds tyok;q laca/kh oh- ,Q ds lkFk izkIr fd, x, oh- ,Q ds vk¡dM+ksa dh rqyuk dh xbZ gSA rhu v{kka’kh; {ks=ksa ¼<16] 16&24] > 24½ ds fy, oh- ,Q- ds fo’ys"k.k ls th- vkbZ- ls 15 % rd dh fHkUurkvksa dk irk pyk gSA o"kkZ&vk/kkfjr Ñf"k okys {ks= esa mYys[kuh; fHkUurk dk irk pyk gSA oh- ,Q- ls izkIr fd, x, ekSleh vkSj o"kZ&izfro"kZ dh fHkUurkvksa ds ifj.kkeksa ij fopkj&foe’kZ fd;k x;k  gSA  Vegetation fraction (VF) is an important input in mesoscale climate models, such as MM5. The most commonly used VF inputs in modeling is the climatic monthly VF generated by Gutman and Ignatov (1998)  (GI) using NOAA-AVHRR NDVI global data sets. This paper reports the generation of 1 km VF data set using SPOT-VEGETATION 10-day composite NDVI products from April 1998 to November 2003 for the Indian region. Sensor-specific thresholds of NDVI associated with 0% and 100% VF for SPOT-VEGETATION were found to be 0.04 and 0.804, respectively, in contrast to 0.04 and 0.52 of GI. Comparison of derived VF with climatic VF of GI was carried out.  Analysis of VF for three latitudinal zones (<16, 16-24, >24) indicated the differences up to 15 percent from GI.  Significant difference was observed for the area having rain-fed agriculture. Results of the seasonal and year-to-year variations of derived VF are discussed.

2016 ◽  
Vol 97 (7) ◽  
pp. 1173-1185 ◽  
Author(s):  
Peter J. Walton ◽  
Morgan B. Yarker ◽  
Michel D. S. Mesquita ◽  
Friederike E. L. Otto

Abstract Globally, decision-makers are increasingly using high-resolution climate models to support policy and planning; however, many of these users do not have the knowledge needed to use them appropriately. This problem is compounded by not having access to quality learning opportunities to better understand how to apply the models and interpret results. This paper discusses and proposes an educational framework based on two independent online courses on regional climate modeling, which addresses the accessibility issue and provides guidance to climate science professors, researchers, and institutions who want to create their own online courses. The role of e-learning as an educational tool is well documented, highlighting the benefits of improved personal efficiency through “anywhere, anytime” learning with the flexibility to support professional development across different sectors. In addition, improved global Internet means increased accessibility. However, e-learning’s function as a tool to support understanding of atmospheric physics and high-resolution climate modeling has not been widely discussed. To date, few courses, if any, support understanding that takes full advantage of e-learning best practices. There is a growing need for climate literacy to help inform decision-making on a range of scales, from individual households to corporate CEOs. And while there is a plethora of climate information online, educational theory suggests that people need to be guided in how to convert this information into applicable knowledge. Here, we present how the experience of the courses we designed and ran independent of each other, both engaging learners with better understanding benefits and limitations of regional climate modeling, lead to a framework of designing e-learning for climate modeling.


2013 ◽  
Vol 2013 ◽  
pp. 1-13 ◽  
Author(s):  
Silvina A. Solman

This review summarizes the progress achieved on regional climate modeling activities over South America since the early efforts at the beginning of the 2000s until now. During the last 10 years, simulations with regional climate models (RCMs) have been performed for several purposes over the region. Early efforts were mainly focused on sensitivity studies to both physical mechanisms and technical aspects of RCMs. The last developments were focused mainly on providing high-resolution information on regional climate change. This paper describes the most outstanding contributions from the isolated efforts to the ongoing coordinated RCM activities in the framework of the CORDEX initiative, which represents a major endeavor to produce ensemble climate change projections at regional scales and allows exploring the associated range of uncertainties. The remaining challenges in modeling South American climate features are also discussed.


2017 ◽  
Vol 14 ◽  
pp. 261-269 ◽  
Author(s):  
Heike Huebener ◽  
Peter Hoffmann ◽  
Klaus Keuler ◽  
Susanne Pfeifer ◽  
Hans Ramthun ◽  
...  

Abstract. Communication between providers and users of climate model simulation results still needs to be improved. In the German regional climate modeling project ReKliEs-De a midterm user workshop was conducted to allow the intended users of the project results to assess the preliminary results and to streamline the final project results to their needs. The user feedback highlighted, in particular, the still considerable gap between climate research output and user-tailored input for climate impact research. Two major requests from the user community addressed the selection of sub-ensembles and some condensed, easy to understand information on the strengths and weaknesses of the climate models involved in the project.


Author(s):  
Erik Kjellström ◽  
Ole Bøssing Christensen

Regional climate models (RCMs) are commonly used to provide detailed regional to local information for climate change assessments, impact studies, and work on climate change adaptation. The Baltic Sea region is well suited for RCM evaluation due to its complexity and good availability of observations. Evaluation of RCM performance over the Baltic Sea region suggests that: • Given appropriate boundary conditions, RCMs can reproduce many aspects of the climate in the Baltic Sea region. • High resolution improves the ability of RCMs to simulate significant processes in a realistic way. • When forced by global climate models (GCMs) with errors in their representation of the large-scale atmospheric circulation and/or sea surface conditions, performance of RCMs deteriorates. • Compared to GCMs, RCMs can add value on the regional scale, related to both the atmosphere and other parts of the climate system, such as the Baltic Sea, if appropriate coupled regional model systems are used. Future directions for regional climate modeling in the Baltic Sea region would involve testing and applying even more high-resolution, convection permitting, models to generally better represent climate features like heavy precipitation extremes. Also, phenomena more specific to the Baltic Sea region are expected to benefit from higher resolution (these include, for example, convective snowbands over the sea in winter). Continued work on better describing the fully coupled regional climate system involving the atmosphere and its interaction with the sea surface and land areas is also foreseen as beneficial. In this respect, atmospheric aerosols are important components that deserve more attention.


2005 ◽  
Vol 5 ◽  
pp. 119-125 ◽  
Author(s):  
S. Kotlarski ◽  
A. Block ◽  
U. Böhm ◽  
D. Jacob ◽  
K. Keuler ◽  
...  

Abstract. The ERA15 Reanalysis (1979-1993) has been dynamically downscaled over Central Europe using 4 different regional climate models. The regional simulations were analysed with respect to 2m temperature and total precipitation, the main input parameters for hydrological applications. Model results were validated against three reference data sets (ERA15, CRU, DWD) and uncertainty ranges were derived. For mean annual 2 m temperature over Germany, the simulation bias lies between -1.1°C and +0.9°C depending on the combination of model and reference data set. The bias of mean annual precipitation varies between -31 and +108 mm/year. Differences between RCM results are of the same magnitude as differences between the reference data sets.


2013 ◽  
Vol 17 (11) ◽  
pp. 4323-4337 ◽  
Author(s):  
M. A. Sunyer ◽  
H. J. D. Sørup ◽  
O. B. Christensen ◽  
H. Madsen ◽  
D. Rosbjerg ◽  
...  

Abstract. In recent years, there has been an increase in the number of climate studies addressing changes in extreme precipitation. A common step in these studies involves the assessment of the climate model performance. This is often measured by comparing climate model output with observational data. In the majority of such studies the characteristics and uncertainties of the observational data are neglected. This study addresses the influence of using different observational data sets to assess the climate model performance. Four different data sets covering Denmark using different gauge systems and comprising both networks of point measurements and gridded data sets are considered. Additionally, the influence of using different performance indices and metrics is addressed. A set of indices ranging from mean to extreme precipitation properties is calculated for all the data sets. For each of the observational data sets, the regional climate models (RCMs) are ranked according to their performance using two different metrics. These are based on the error in representing the indices and the spatial pattern. In comparison to the mean, extreme precipitation indices are highly dependent on the spatial resolution of the observations. The spatial pattern also shows differences between the observational data sets. These differences have a clear impact on the ranking of the climate models, which is highly dependent on the observational data set, the index and the metric used. The results highlight the need to be aware of the properties of observational data chosen in order to avoid overconfident and misleading conclusions with respect to climate model performance.


2017 ◽  
Vol 30 (5) ◽  
pp. 1605-1627 ◽  
Author(s):  
Pengfei Xue ◽  
Jeremy S. Pal ◽  
Xinyu Ye ◽  
John D. Lenters ◽  
Chenfu Huang ◽  
...  

Abstract Accurate representations of lake–ice–atmosphere interactions in regional climate modeling remain one of the most critical and unresolved issues for understanding large-lake ecosystems and their watersheds. To date, the representation of the Great Lakes two-way interactions in regional climate models is achieved with one-dimensional (1D) lake models applied at the atmospheric model lake grid points distributed spatially across a 2D domain. While some progress has been made in refining 1D lake model processes, such models are fundamentally incapable of realistically resolving a number of physical processes in the Great Lakes. In this study, a two-way coupled 3D lake-ice–climate modeling system [Great Lakes–Atmosphere Regional Model (GLARM)] is developed to improve the simulation of large lakes in regional climate models and accurately resolve the hydroclimatic interactions. Model results are compared to a wide variety of observational data and demonstrate the unique skill of the coupled 3D modeling system in reproducing trends and variability in the Great Lakes regional climate, as well as in capturing the physical characteristics of the Great Lakes by fully resolving the lake hydrodynamics. Simulations of the climatology and spatiotemporal variability of lake thermal structure and ice are significantly improved over previous coupled, 1D simulations. At seasonal and annual time scales, differences in model results are primarily observed for variables that are directly affected by lake surface temperature (e.g., evaporation, precipitation, sensible heat flux) while no significant differences are found in other atmospheric variables (e.g., solar radiation, cloud cover). Underlying physical mechanisms for the simulation improvements using GLARM are also discussed.


2007 ◽  
Vol 88 (9) ◽  
pp. 1395-1410 ◽  
Author(s):  
Jeremy S. Pal ◽  
Filippo Giorgi ◽  
Xunqiang Bi ◽  
Nellie Elguindi ◽  
Fabien Solmon ◽  
...  

Regional climate models are important research tools available to scientists around the world, including in economically developing nations (EDNs). The Earth Systems Physics (ESP) group of the Abdus Salam International Centre for Theoretical Physics (ICTP) maintains and distributes a state-of-the-science regional climate model called the ICTP Regional Climate Model version 3 (RegCM3), which is currently being used by a large research community for a diverse range of climate-related studies. The RegCM3 is the central, but not only, tool of the ICTP-maintained Regional Climate Research Network (RegCNET) aimed at creating south–south and north–south scientific interactions on the topic of climate and associated impacts research and modeling. In this paper, RegCNET, RegCM3, and illustrative results from RegCM3 benchmark simulations applied over south Asia, Africa, and South America are presented. It is shown that RegCM3 performs reasonably well over these regions and is therefore useful for climate studies in EDNs.


2020 ◽  
Vol 101 (5) ◽  
pp. E664-E683 ◽  
Author(s):  
W. J. Gutowski ◽  
P. A. Ullrich ◽  
A. Hall ◽  
L. R. Leung ◽  
T. A. O’Brien ◽  
...  

ABSTRACT Regional climate modeling addresses our need to understand and simulate climatic processes and phenomena unresolved in global models. This paper highlights examples of current approaches to and innovative uses of regional climate modeling that deepen understanding of the climate system. High-resolution models are generally more skillful in simulating extremes, such as heavy precipitation, strong winds, and severe storms. In addition, research has shown that fine-scale features such as mountains, coastlines, lakes, irrigation, land use, and urban heat islands can substantially influence a region’s climate and its response to changing forcings. Regional climate simulations explicitly simulating convection are now being performed, providing an opportunity to illuminate new physical behavior that previously was represented by parameterizations with large uncertainties. Regional and global models are both advancing toward higher resolution, as computational capacity increases. However, the resolution and ensemble size necessary to produce a sufficient statistical sample of these processes in global models has proven too costly for contemporary supercomputing systems. Regional climate models are thus indispensable tools that complement global models for understanding physical processes governing regional climate variability and change. The deeper understanding of regional climate processes also benefits stakeholders and policymakers who need physically robust, high-resolution climate information to guide societal responses to changing climate. Key scientific questions that will continue to require regional climate models, and opportunities are emerging for addressing those questions.


2019 ◽  
pp. 127-139
Author(s):  
Tatjana Ratknić ◽  
Mihailo Ratknić ◽  
Lazar Vukadinović

Regional climate modelling with regional climate models has become a part of modern research with a wide range of applications. This article examines the latest segments in the study of regional climate modeling used to assess the adaptivity and survival of particular forest species in changing conditions. It presents the results of the regional climate model (acronym REG-IN) used to predict the adaptive capacity of forest ecosystems in Belgrade. Compared to the SXG and E-P models, the REG-IN model exhibits certain deviations due to the specific environmental conditions of the area. These data have made it possible to predict the future rate of survival of individual forest ecosystems


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