Gotowe bibliografie tematyczne / Climate change- Northwest India

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Gotowa bibliografia na temat „Climate change- Northwest India”

Autor: Grafiati

Data publikacji: 6 września 2023

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Artykuły w czasopismach na temat "Climate change- Northwest India"

Yadav, R. K., K. Rupa Kumar i M. Rajeevan. "Climate change scenarios for Northwest India winter season". Quaternary International 213, nr 1-2 (luty 2010): 12–19. http://dx.doi.org/10.1016/j.quaint.2008.09.012.

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RATHORE, L. S., K. K. SINGH, S. A. SASEENDRAN i A. K. BAXLA. "Modelling the impact of climate change on rice production in India". MAUSAM 52, nr 1 (29.12.2021): 263–74. http://dx.doi.org/10.54302/mausam.v52i1.1693.

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The CERES-Rice crop simulation model, calibrated and validated for the varieties PR106 in NW India. IR36 in central India and Jaya in south India, is used for nalysing the effect of climate change on rice productivity in the country. Plausible climate change scenario for the Indian subcontinent as expected by the middle of the next century taking into account the projected emissions of greenhouse gases and sulphate aerosols, in a coupled atmosphere-ocean model experiment performed at Deutsches Klimarechenzentrum, Germany, is adopted for the study. The adopted scenario represented an increase in monsoon seasonal mean surface temperature of the order of about 1.5° C over the south India and 1°C over northwest and central India in the decade 2040-49 with respect to the 1980s and an increase in rainfall of the order of 2 mm per day over south India while the simulated decrease of the order about -1 mm and -1.5 mm over northwest and central India respectively. The IPCC Business-as-usual scenario projection of plant usable concentration of CO2 about 460 PPM by the middle fo the next century are also used in the crop model simulation (CERES - Rice V3 Model). Simulation studies carried out with the climate change scenarios over different parts of the country are analysed and interpreted.

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V.P. PRAMOD, B. BAPUJI RAO, S.S.V.S. RAMAKRISHNA, M. MUNESHWAR SINGH, N.R. PATEL, V.M. SANDEEP, V.U.M. RAO, P. S. CHOWDARY, V. NARSIMHA RAO i P. VIJAYA KUMAR. "Impact of projected climate on wheat yield in India and its adaptation strategies". Journal of Agrometeorology 19, nr 3 (1.09.2017): 207–16. http://dx.doi.org/10.54386/jam.v19i3.627.

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Wheat is highly sensitive to climate change especially temperature changes experienced in the later phase of crop season. Hence, it is of immense importance to know how and to what extent climate change will affect wheat yields and to assess the adaptive strategies for mitigating possible negative consequences on wheat production. Wheat yield responses to three future climatic periods (2025, 2050 and 2075) were studied by driving DSSAT-Wheat (v4.5) model with daily weather from three CMIP-5 climate models’ (GFDL-ESM2M, MIROC5, and NorESM1-M) as the basic input at four sites (Ludhiana, Raipur, Akola and New Delhi) representing three major wheat growing zones of the country. Projected changes in growing season (November-March) day and night temperatures at four sites differed substantially both in direction and magnitude. Day temperatures are projected to rise conspicuously at Ludhiana, representing northwest parts of the country, and moderately over central parts of India (Akola and Raipur). Positive rainfall anomalies at Ludhiana (+76%) and negative anomalies at Raipur (-15%) are projected in future climates. With these anticipated changes, wheat is likely to experience warmer days (+1.1 °C) at Ludhiana and nights at Raipur (+2.8 °C) and more seasonal moisture availability at Ludhiana in future climates. Negative impacts of climatic change in these sites are found to be minimized by adapting one or a combination of management practices, which are site specific.

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van Oldenborgh, Geert Jan, Sjoukje Philip, Sarah Kew, Michiel van Weele, Peter Uhe, Friederike Otto, Roop Singh, Indrani Pai, Heidi Cullen i Krishna AchutaRao. "Extreme heat in India and anthropogenic climate change". Natural Hazards and Earth System Sciences 18, nr 1 (24.01.2018): 365–81. http://dx.doi.org/10.5194/nhess-18-365-2018.

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Abstract. On 19 May 2016 the afternoon temperature reached 51.0 °C in Phalodi in the northwest of India – a new record for the highest observed maximum temperature in India. The previous year, a widely reported very lethal heat wave occurred in the southeast, in Andhra Pradesh and Telangana, killing thousands of people. In both cases it was widely assumed that the probability and severity of heat waves in India are increasing due to global warming, as they do in other parts of the world. However, we do not find positive trends in the highest maximum temperature of the year in most of India since the 1970s (except spurious trends due to missing data). Decadal variability cannot explain this, but both increased air pollution with aerosols blocking sunlight and increased irrigation leading to evaporative cooling have counteracted the effect of greenhouse gases up to now. Current climate models do not represent these processes well and hence cannot be used to attribute heat waves in this area. The health effects of heat are often described better by a combination of temperature and humidity, such as a heat index or wet bulb temperature. Due to the increase in humidity from irrigation and higher sea surface temperatures (SSTs), these indices have increased over the last decades even when extreme temperatures have not. The extreme air pollution also exacerbates the health impacts of heat. From these factors it follows that, from a health impact point of view, the severity of heat waves has increased in India. For the next decades we expect the trend due to global warming to continue but the surface cooling effect of aerosols to diminish as air quality controls are implemented. The expansion of irrigation will likely continue, though at a slower pace, mitigating this trend somewhat. Humidity will probably continue to rise. The combination will result in a strong rise in the temperature of heat waves. The high humidity will make health effects worse, whereas decreased air pollution would decrease the impacts.

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Arumugam, Surendran, Ashok K.R., Suren N. Kulshreshtha., Isaac Vellangany i Ramu Govindasamy. "Yield variability in rainfed crops as influenced by climate variables". International Journal of Climate Change Strategies and Management 7, nr 4 (16.11.2015): 442–59. http://dx.doi.org/10.1108/ijccsm-08-2013-0096.

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Purpose – This paper aims to explore the impact of climate change on yields and yield variances in major rainfed crops and measure possible changes in yields under projected climate changes in different agro-climatic zones of Tamil Nadu, India. Although many empirical studies report the influence of climate change on crop yield, only few address the effect on yield variances. Even in such cases, the reported yield variances were obtained through simulation studies rather than from actual observations. In this context, the present study analyzes the impact of climate change on crops yield and yield variance using the observed yields. Design/methodology/approach – The Just-Pope yield function (1978) is used to analyze the impact of climate change on mean yield and variance. The estimated coefficient from Just-Pope yield function and the projected climatic data for the year 2030 are incorporated to capture the projected changes in crop yield and variances. Findings – By the year 2030, the yield of pulses is estimated to decline in all the zones (Northeast, Northwest, Western, Cauvery delta, South and Southern zones), with significant declines in the Northeast zone (6.07 per cent), Cauvery delta zone (3.55 per cent) and South zone (3.54 per cent). Sorghum yield may suffer more in Western zone (2.63 per cent), Southern zone (1.92 per cent) and Northeast zone (1.62 per cent). Moreover, the yield of spiked millet is more likely to decrease in the Southern zone (1.39 per cent), Northeast zone (1.21 per cent) and Cauvery delta zone (0.24 per cent), and the yield of cotton may also decline in the Northeast zone (12.99 per cent), Northwest zone (8.05 per cent) and Western zone (2.10 per cent) of Tamil Nadu, India. Originality/value – The study recommends introducing appropriate crop insurance policies to address possible financial losses to the farmers. Prioritizing area-specific stress-tolerant crop varieties without complementing yield would sustain crops cultivation further.

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Mira Shivani, S., S. Srivastava i A. Singh. "Critical analysis of hydrological mass variations of northwest India". IOP Conference Series: Earth and Environmental Science 1032, nr 1 (1.06.2022): 012032. http://dx.doi.org/10.1088/1755-1315/1032/1/012032.

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Abstract With current climate change, water availability is a huge concern. Ground-water (GW) is depleting at a steep rate globally and more specifically in Northwest India. Estimation and analysis of GW availability would be of great use for formulating a proper water management plan for the future. The study is carried out in the north-western part of India with the aim of generating a time series for total water storage (TWS) using different remote sensing and model-based data like GRACE, Landsat, MODIS. From the time series, it is clear-cut that, the TWS is showing a declining trend and this might be due to depletion of groundwater as, other variables like precipitation, evapotranspiration, soil moisture (obtained from MERRA-2 and CFSR data) are not showing any negative trend during the study period (2002 - 2021). Also, from the change detection analysis of land use land cover maps and crop yield statistics of water-intensive crops it can be concluded that croplands in the study area are increasing denoting the usage of water for irrigation at a large scale. Thus, better management of the groundwater is required for avoiding severe water scarcity in the future.

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Petrie, Cameron A., Ravindra N. Singh, Jennifer Bates, Yama Dixit, Charly A. I. French, David A. Hodell, Penelope J. Jones i in. "Adaptation to Variable Environments, Resilience to Climate Change: InvestigatingLand, Water and Settlementin Indus Northwest India". Current Anthropology 58, nr 1 (2.02.2017): 1–30. http://dx.doi.org/10.1086/690112.

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Vu, Quyet Manh, i Tri Dan Nguyen. "Agroforestry Suitability Mapping for the Northwest Provinces of Vietnam". Proceedings 36, nr 1 (3.04.2020): 142. http://dx.doi.org/10.3390/proceedings2019036142.

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This study aims to assess the potential development of selected agroforestry options for three provinces in the Northwest of Vietnam. Available spatial data including Land use/land cover maps and forest inventory maps were used as the base maps in combination with supplementary data and field survey to determine the potential agroforestry areas. Soil types, soil depth, soil texture, elevation, slope, temperature and rainfall were used to evaluate the biophysical suitability of ten typical agroforestry options in the study region. For assessing the impact of climate change to agroforestry suitability in the future, temperature and precipitation data extracted from two climate changes scenarios (Representative Concentration Pathway 4.5 and 8.5 in 2046–2065) were used. The results showed that the suitable areas for agroforestry development in Dien Bien, Sơn La and Yen Bai provinces were 267.74.01 ha, 405,597.96 ha; and 297,995.55 ha, respectively. Changes in temperature and precipitation by 2 climate change scenarios affected significantly to the suitability of Docynia indica + livestock grass, Teak + plum + coffee + grass and Plum + maize + livestock grass options. The map of agroforestry suitability can be served as a useful source in developing and expanding the area of agroforestry in the target provinces, and can be applied for other provinces in the same region in Vietnam.

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Phartiyal, Binita, Sheikh Nawaz Ali, Anupam Sharma, Shailesh Agrawal, Debarati Nag, Pooja Tiwari, Mohan Kumar i in. "Palaeoclimatic variability during last eight millennia from a morainal lake in Zanskar, northwest Himalaya, India". Journal of Palaeosciences 71, nr 1 (22.07.2022): 75–88. http://dx.doi.org/10.54991/jop.2022.545.

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Centennial–scale palaeoenvironmental variability has been deduced during past eight millennia using multi–proxy study (textural analysis, environmental magnetic parameters, stable carbon isotopes, palynofacies and elemental concentration), from Khangok–Padam in Zanskar Valley, northwest Himalaya. The multi–proxy record from this morainal lake spanning last ~8200 cal years BP has revealed four hydroclimatic phases. The overall progressively improving hydroclimatic trend is indicated by multi proxy study: sediment size/texture (as a proxy for the energy condition and depositional environment), mineral magnetism (proxy for sediment flux or lithogenic input and lithologic variation), carbon isotope signature (δ13Corg) preserved in organic constituents of sediments (a proxy for palaeovegetation and climate change), elemental geochemistry (proxy for weathering and erosion) and selected samples for palynofacies data (a proxy for changes in biological organic matter). This improving hydroclimatic trend is however punctuated by an abrupt wet spell at ~6200–5200 cal years BP and relatively drier climate during the Little Ice Age between 1400 and 1900 CE. The main driving force implicated for the changes are seen to be the solar output variations. The area lying in a transitional climatic zone of NW Himalaya shows no emphatic record of the events like the 4200 cal. years BP, 2600 cal. years BP and Holocene Climatic Optima. Contrary to the earlier studies in the region (e.g., Tsokar and TsoMorari), our results show an improving hydroclimatic condition in this transition climatic zone between the Indian Summer Monsoon dominated Higher and westerly dominated Trans Himalaya.

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Mukherjee, Avik, S. Y. Wang i Parichart Promchote. "Examination of the Climate Factors That Reduced Wheat Yield in Northwest India during the 2000s". Water 11, nr 2 (18.02.2019): 343. http://dx.doi.org/10.3390/w11020343.

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In India, a significant reduction of wheat yield would cause a widespread impact on food security for 1.35 billion people. The two highest wheat producing states, Punjab and Haryana in northern India, experienced a prolonged period of anomalously low wheat yield during 2002–2010. The extent of climate variability and change in influencing this prolonged reduction in wheat yield was examined. Daily air temperature (Tmax and Tave) was used to calculate the number of days above optimum temperature and growing degree days (GDD) anomaly. Two drought indices, the standard precipitation and evapotranspiration index and the radiation-based precipitation index, were used to describe the drought conditions. Groundwater variability was assessed via satellite-based approximation. The analysis results indicate that the wheat yield loss corresponds to the increase in the number of days with a temperature above 35 °C during the maturity stage (March). Reduction in monsoon rainfall led to a depletion of groundwater and reduced surface water for irrigation in the wheat growing season (November–March). Higher temperatures, coupled with water shortage and irregular irrigation, also appear to impact the yield reduction. In hindsight, improving the agronomic practices to minimize crop water usage could be an adaptation strategy to maintain the desired wheat yield in the face of climate-induced drought and precipitation anomaly.

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Rozprawy doktorskie na temat "Climate change- Northwest India"

Cromack, Marianne. "A glacial sedimentary system in northwest Spitzbergen". Thesis, University of Cambridge, 1991. https://www.repository.cam.ac.uk/handle/1810/268051.

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The record of climate change in Signedalen and Krossfjorden, northwest Spitsbergen, since the Late Weichselian glacial maximum, has been constructed using an integrated analysis of lacustrine, terrestrial and marine sediments. Thirty-four piston cores were taken from two series of linked lakes in Signedalen, fed by three small cirque glaciers. Six further cores were taken from the fjord inlet, Signehamna, into which meltwater from the linked glacier-fed lakes and a further two glaciers drain. Signehamna drains into Lilliehookfjorden, which with Mollerfjorden, combines to form Krossfjorden, from which 16 .cores were made available. Cores were analysed for moisture content, loss-on-ignition, bulk density, grain size, magnetic susceptibility, infra-red stimulated luminescence, by X-radiography and by radioisotopic dating methods, 210Pb and 14C. Bathymetric maps were constructed following echo sounding survey of the lakes. Seventy-two water samples from the linked lakes were used to assess contemporary environmental conditions, and to aid interpretation of sedimentary structures within core sediments. Results of lichenometric survey of moraine ridges and pro-talus deposits in and around Signedalen were analysed using discriminant analysis, and compared with Werner's (1988) lichen growth curve in order to establish a chronology of moraine stabilisation. Seismic records of Krossfjorden have revealed evidence of glacier advance at least as far as the sill separating Krossfjorden from the outer parts of the fjord and shelf associated with the Late Weichselian glacial maximum (Sexton et al., in press). Overlying the basal unit of a possible till , or sediments associated with rapid glacier retreat, is a blanket of homogeneous sediment formed by ice-distal deposition during the Holocene. There is no evidence of Younger Dryas glacier expansion preserved in the marine sediments, or in terrestrial moraines. Denudation rates calculated from lacustrine sediment accumulation infer the presence of smaller glaciers in Signedalen during the Younger Dryas than at present. The early to mid Holocene appears to have been characterised by relatively warm conditions, with much reduced glacier presence in Signedalen. Evidence of Neoglacial cooling, between approximately 3,000 yr BP and 1,500 yr BP, is found in lichenometric recorckof talus deposits, although precise dating of the inception, and duration of this cooling is problematic. No moraine sediments are recorded from this period. The Little Ice Age maximum, dated by licheno~etry to AD 1890, was the most extensive glacier advance to have affected the cirque glaciers of Signedalen and the tidewater glaciers of Krossfjorden, and is associated with the highest denudation rates recorded in the lacustrine sediments. It also appears to have been responsible for the formation of rock glaciers within the protalus deposits of Signedalen. Since this date, a general retreat of glaciers has been interrupted periodically by still-stands or slight readvances when climatic conditions deteriorated.

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Najafi, Mohammad Reza. "Climate Change Impact on the Spatio-Temporal Variability of Hydro-Climate Extremes". PDXScholar, 2013. https://pdxscholar.library.pdx.edu/open_access_etds/1114.

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The rising temperature of the earth due to climate change has shown to alter the variations of hydro-climate variables, including their intensities, frequencies and durations. Extreme events such as floods are, in particular, susceptible to any disturbances in climate cycles. As such it is important to provide policymakers with sufficient knowledge about the probable impacts of climate change on hydrologic extremes and most importantly on floods, which have the highest impacts on the societies. For this reason analysis of hydro-climate extremes is commonly performed using data at each site (or grid cell), however due to the limited number of extreme events, these analyses are not robust. Current methods, such as the regional frequency analysis, which combine data from different locations are incapable of incorporating the spatial structure of the data as well as other explanatory variables, and do not explicitly, assess the uncertainties. In this thesis the spatial hierarchical Bayesian model is proposed for hydro-climate extreme analyses using data recorded at each site or grid. This method combines limited number of data from different locations, estimates the uncertainties in different stages of the hierarchy, incorporates additional explanatory variables (covariates), and can be used to estimate extreme events at un-gaged sites. The first project develops a spatial hierarchical Bayesian method to model the extreme runoffs over two spatial domains in the Columbia River Basin, U.S. The model is also employed to estimate floods with different return levels within time slices of fifteen years in order to detect possible trends in runoff extremes. Continuing on the extreme analysis, the impact of climate change on runoff extremes is investigated over the whole Pacific Northwest (PNW). This study aims to address the question of how the runoff extremes will change in the future compared to the historical time period, investigate the different behaviors of the regional climate models (RCMs) regarding the runoff extremes, and assess the seasonal variations of runoff extremes. Given the increasing number of climate model simulations the goal of the third project is to provide a multi-model ensemble average of hydro-climate extremes and characterize the inherent uncertainties. Outputs from several regional climate models provided by NARCCAP are considered for the analysis in all seasons. Three combination scenarios are defined and compared for multi-modeling of extreme runoffs. The biases of each scenario are calculated and the scenario with the least bias is selected for projecting seasonal runoff extremes. The aim of the fourth project is to quantify and compare the uncertainties regarding global climate models to the ones from the hydrologic model structures in climate change impact studies. Various methods have been proposed to downscale the coarse resolution General Circulation Model (GCM) climatological variables to the fine scale regional variables; however fewer studies have been focused on the selection of GCM predictors. Additionally, the results obtained from one downscaling technique may not be robust and the uncertainties related to the downscaling scheme are not realized. To address these issues, in the fifth study we employed Independent Component Analysis (ICA) for predictor selection which determines spatially independent GCM variables (as discussed in Appendix A). Cross validation of the independent components is employed to find the predictor combination that describes the regional precipitation over the upper Willamette basin with minimum error. These climate variables along with the observed precipitation are used to calibrate three downscaling models: Multi Linear Regression (MLR), Support Vector Machine (SVM) and Adaptive-Network-Based Fuzzy Inference System (ANFIS).

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Manuvie, Ritumbra. "Governance of climate change related migrations in Assam (India)". Thesis, University of Edinburgh, 2018. http://hdl.handle.net/1842/31147.

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The thesis asks two crucial questions, (a) what are the normative frameworks available for protecting the rights and status of a person migrating due to climate change related hydro-metrological changes? (b) why is there a non-uniformity and inadequacy in the deliverance of assistance from the state? To address these questions, I have analysed the perception, framing and assistance a climate change migrant receives from the state of Assam in India, while also explaining the reasons for the differential nature and deficits in protection. Based on interviews with senior bureaucratic officials (elite actors), group-discussions, field surveys, and engagements at the block and village level, the thesis makes three critical arguments. First, the sub-national government perceive climate-induced migrations as a developmental issue. Second, the way in which climate change migration is framed as a developmental issue by elite actors does not correspond with how the issue is understood by street-level bureaucratic actors. Instead, the routine judgements and discretions exercised by street-level actors are complexly tied to the political and social circumstances of local areas. Finally, while it is known that socio-political and demographic factors (such as gender, membership of a social group, and religion) contribute to forced forms of migration, the thesis argues that these demographic factors also adversely affect the performance of the programs meant to reduce climate vulnerabilities.

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Bookhagen, Bodo. "Late quaternary climate changes and landscape evolution in the Northwest Himalaya geomorphologic processes in the Indian summer monsoon domain /". Phd thesis, [S.l. : s.n.], 2004. http://deposit.ddb.de/cgi-bin/dokserv?idn=974115487.

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Dimitrova, Asya 1988. "Climate change and health in India : impacts and co-benefits". Doctoral thesis, TDX (Tesis Doctorals en Xarxa), 2022. http://hdl.handle.net/10803/673181.

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El primer estudio de esta tesis doctoral demostró que tanto las temperaturas ambientales altas como las bajas y las olas de calor son factores de riesgo de mortalidad por todas las causas en la India, y el riesgo de mortalidad aumenta de manera más pronunciada a temperaturas más altas. El segundo y tercer estudio evaluaron algunos de los beneficios colaterales para la salud relacionados con la contaminación del aire y las compensaciones de la mitigación del cambio climático en la India. Los hallazgos sugirieron que la reducción proyectada de la contaminación del aire ambiental bajo los objetivos del Acuerdo de París puede alargar la esperanza de vida al nacer, reducir la mortalidad prematura y el número de niños con retraso en el crecimiento en la India para 2050 en comparación con los negocios habituales. Sin embargo, los costos de combustible más altos en virtud de los objetivos del Acuerdo de París pueden conducir a una mayor contaminación del aire en los hogares, compensando así por completo los beneficios para el crecimiento lineal infantil de una mejor calidad del aire ambiental. Complementar las medidas de mitigación con el control de la calidad del aire al final de la tubería y las políticas para respaldar el acceso a una cocina limpia puede maximizar los beneficios colaterales para la salud y reducir las compensaciones de mitigación, especialmente entre los más desfavorecidos.
The first study in this PhD thesis demonstrated that both high and low ambient temperatures and heatwaves are risk factors for all-cause mortality in India, with mortality risk increasing more steeply at higher temperatures. The second and third study assessed some of the air pollution related health co-benefits and trade-offs from climate change mitigation in India. Findings suggested that projected reduction of ambient air pollution under the Paris Agreement targets can lengthen life expectancy at birth, reduce premature mortality and the number of stunted children in India by 2050 compared to the business-as-usual. However, higher fuel costs under Paris Agreement targets can lead to higher household air pollution, thus completely offsetting the benefits for child linear growth from improved ambient air quality. Complementing mitigation measures with end-of-pipe air quality control and policies to support access to clean cooking can maximise health co-benefits and reduce mitigation trade-offs, especially among the most disadvantaged.

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Andrews, Christopher James. "Human responses to climate change during the Younger Dryas in Northwest Europe". Thesis, University of Cambridge, 2018. https://www.repository.cam.ac.uk/handle/1810/276744.

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This study discusses the extent to which hunter-gatherer mobility strategies are changed by abrupt climate change events by monitoring changes in lithic assemblage compositions through the Pleistocene/Holocene Transition, from ca. 14,000 cal BP to 10,000 cal BP in northwest Europe, with a focus on the Younger Dryas Stadial event, which occurred around 12,900 cal BP to 11,700 cal BP. A set of predicted archaeological indicators were formed from existing theoretical models, based largely on Binford’s logistical and residential mobility model, with the expectation that a more residential mobility strategy would be used by hunter-gatherer-populations during warmer climatic phases (i.e. the Allerød and Preboreal) and a more logistical mobility strategy would be used during cold climatic phases (i.e. the Younger Dryas). The lithic assemblages from sites across northwest Europe were then compared with these expectations in order to determine if a shift from a more residential strategy to a more logistical strategy can be seen from the lithic record. Additionally, a further comparative dataset was collected from south Europe in order to determine if there were differences in the response to the Younger Dryas at lower latitudes where the impact of this event is assumed to be less severe. The results found that in northwest Europe there is evidence to suggest there was indeed a shift from a more residential strategy during the warm Allerød interstadial to a more logistical strategy during the Younger Dryas Stadial, and the adoption of a more residential strategy with the return of warmer conditions during the Preboreal. However, it appears that the Preboreal Interstadial shows significant differences between the Allerød Interstadial, with the Preboreal sharing more characteristics in common with the Younger Dryas. This has been interpreted as a response to the unstable climatic conditions reported from the environmental evidence in this region during the Preboreal, which may have limited the ability of hunter-gatherer populations to return to similar levels of residential mobility seen during the Allerød. The south Europe dataset provides evidence that the lesser impact of the Younger Dryas at lower latitudes brought about a more muted response by hunter-gatherer populations to this event when compared with the northwest. However, there appears to be a reversal of that seen in the northwest, with more logistically mobile populations during the Allerød and especially the Preboreal, and more residentially mobile populations during the Younger Dryas. This is despite the environmental evidence showing a very similar environmental response to the northwest, with a distinct opening of the landscape during the Younger Dryas. The apparent difference in mobility strategies appear to be more related to the available faunal species within a region and their behaviour within their environment rather than directly to the climate. In the south, species such as red deer and ibex are the main source of faunal subsistence throughout the Pleistocene/Holocene Transition, unchanged by shifts in temperature and environment, but the way in which hunter-gatherers would hunt such species would be expected to change in more wooded environments compared with more open environments. If we compare this with the northwest, there is evidence of a distinct change from hunted prey, such as red deer, during the Allerød and Preboreal, to reindeer and horse during the Younger Dryas (although faunal preservation is poor in this region). With this shift to a more mobile prey species, along with a harsher, more open environment it may be more suitable to practise a more logistical strategy. Additionally, the instability of the Preboreal may have also changed the environment on a smaller scale, which would have required the hunting of warmer climate prey in shifting local environments, much like that of the Younger Dryas in south Europe. This might explain the differences seen between the Allerød and the Preboreal. Overall, there appears to be strong evidence supporting the theory that colder, harsher climates promote a more logistically mobile response from hunter-gatherer populations as seen in the northwest of Europe, and that there was a more muted, different response to the Younger Dryas in the lower latitudes of south Europe. However, it is the opinion here that changes in human mobility are not controlled directly be climatic conditions, rather controlled by the available major prey species and their behaviour in changing environments.

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Szczurek, Anthony. "India's Temporal Imaginaries of Climate Change, 1988-2018". Diss., Virginia Tech, 2019. http://hdl.handle.net/10919/88984.

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The advent of climate change promises extreme disruptions to existing concepts of political time, namely the distinction between the modes of time adopted by modern nation-states, natural time, and the everyday life of human beings. Yet the nation-state remains the primary actor through which climate politics is shaped. India is one the most prominent actors in the UN Framework Convention on Climate Change (UNFCCC) and also likely to be one of the most climate-affected societies moving forward. Over the 30-year history of India's engagement at the UNFCCC, there has been a shift from constructing a secular, past-oriented imaginary to a sacred, future-oriented one. The state has fostered these temporal imaginaries through three discursive registers: international politics, climate science, and conservative Hindu ideology. These imaginaries act as a heuristic tool with which to analyze the changing dynamics of political temporality in an era of rapid and extreme climate change.
Doctor of Philosophy
Climate change challenges fundamental notion of political time, the temporal relationship that embeds actors and processes. Yet this topic is underanalyzed in academic literature, especially when it comes to non-Western states. India has been one of the most prominent actors at the United Nations climate negotiations and also likely to be heavily affected by extreme climate shifts. Over the 30-year history of the UN Framework Convention on Climate Change (UNFCCC), the Indian government has framed the temporality of climate change in two ways. First, from 1988-2004, it constructed and followed a secular, past-oriented imaginary of climate change. Beginning in 2005, and accelerating with the election of Prime Minister Modi in 2014, the government has begun to construct and follow a sacred, future-oriented imaginary. In this way, the State has moved from rhetorically framing climate change as a significant problem to an opportunity that can be met if India and other societies follow conservative Hindu precepts.

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Wilson, Hannah. "Climate Change Effects on Arbuscular Mycorrhizal Fungi and Prairie Plants Along a Mediterranean Climate Gradient". Thesis, University of Oregon, 2013. http://hdl.handle.net/1794/12968.

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Arbuscular mycorrhizal fungi (AMF) provide numerous services to their plant symbionts. Understanding the effects of climate change on AMF, and the resulting plant responses, is a crucial factor in predicting ecosystem responses on a global scale. We used a manipulative climate change experiment embedded within a natural climate gradient in Oregon and Washington to examine how the effects of future climate change on AMF-plant symbioses are mediated by soil water availability, soil nutrient availability, and vegetation dynamics. Using structural equation modeling, we found that the direct effect of increasing temperatures was to decrease AMF colonization. Indirect effects of temperature, mediated through other variables, canceled each other out. However, future shifts in these relationships could either exacerbate or mitigate the negative direct effect of temperature. As ecosystems in Mediterranean climates experience more intense droughts and heavier rains, decreases in AMF colonization could have substantial consequences for plant communities and ecosystem function.

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Freeland, Ballantyne Erin. "Sustainability's paradox : community health, climate change and petrocapitalism". Thesis, University of Oxford, 2013. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.711671.

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Fisher, Susannah Emily. "Networks for climate change : non-state and subnational actors in Indian climate politics and governance". Thesis, University of Cambridge, 2012. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.610233.

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Książki na temat "Climate change- Northwest India"

Dalton, Meghan M., Philip W. Mote i Amy K. Snover, red. Climate Change in the Northwest. Washington, DC: Island Press/Center for Resource Economics, 2013. http://dx.doi.org/10.5822/978-1-61091-512-0.

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Narain, Sunita. Climate change: Perspectives from India. New Delhi: UNDP, 2009.

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Narain, Sunita. Climate change: Perspectives from India. New Delhi: Uited Nations Development Programme, India, 2009.

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Narain, Sunita. Climate change: Perspectives from India. New Delhi: Uited Nations Development Programme, India, 2009.

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Narain, Sunita. Climate change: Perspectives from India. New Delhi: UNDP, 2009.

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Gallagher, Denise M. Implications of climate change in India. New York: Nova Science Publishers, Inc., 2011.

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Carothers, Courtney. Climate change and subsistence fisheries in northwest Alaska. Anchorage, Alaska]: U.S. Fish and Wildlife Service, Office of Subsistence Management, Fisheries Resource Monitoring Program, 2013.

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Centre for Environment Education (Ahmadābād, India), red. Climate change: An Indian perspective. New Delhi: Cambridge University Press, India [and] Centre for Envrionment Education, Ahmedabad, 2007.

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Meyer-Ohlendorf, Lutz. Drivers of Climate Change in Urban India. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-96670-0.

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Malini, Mehra, i Centre for Social Markets (Calcutta, India), red. Who's who in climate change in India. Kolkata: Centre for Social Markets, 2008.

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Części książek na temat "Climate change- Northwest India"

Lynn, Kathy, Oliver Grah, Preston Hardison, Jennie Hoffman, Ed Knight, Amanda Rogerson, Patricia Tillmann, Carson Viles i Paul Williams. "Northwest Tribes". W Climate Change in the Northwest, 207–30. Washington, DC: Island Press/Center for Resource Economics, 2013. http://dx.doi.org/10.5822/978-1-61091-512-0_8.

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Mote, Philip W., John T. Abatzoglou i Kenneth E. Kunkel. "Climate". W Climate Change in the Northwest, 25–40. Washington, DC: Island Press/Center for Resource Economics, 2013. http://dx.doi.org/10.5822/978-1-61091-512-0_2.

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Pink, Ross Michael. "India". W The Climate Change Crisis, 163–84. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-71033-4_7.

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Snover, Amy K., Patty Glick i Susan M. Capalbo. "Introduction". W Climate Change in the Northwest, 1–24. Washington, DC: Island Press/Center for Resource Economics, 2013. http://dx.doi.org/10.5822/978-1-61091-512-0_1.

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Raymondi, Rick R., Jennifer E. Cuhaciyan, Patty Glick, Susan M. Capalbo, Laurie L. Houston, Sarah L. Shafer i Oliver Grah. "Water Resources". W Climate Change in the Northwest, 41–66. Washington, DC: Island Press/Center for Resource Economics, 2013. http://dx.doi.org/10.5822/978-1-61091-512-0_3.

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Reeder, W. Spencer, Peter Ruggiero, Sarah L. Shafer, Amy K. Snover, Laurie L. Houston, Patty Glick, Jan A. Newton i Susan M. Capalbo. "Coasts". W Climate Change in the Northwest, 67–109. Washington, DC: Island Press/Center for Resource Economics, 2013. http://dx.doi.org/10.5822/978-1-61091-512-0_4.

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Littell, Jeremy S., Jeffrey A. Hicke, Sarah L. Shafer, Susan M. Capalbo, Laurie L. Houston i Patty Glick. "Forest Ecosystems". W Climate Change in the Northwest, 110–48. Washington, DC: Island Press/Center for Resource Economics, 2013. http://dx.doi.org/10.5822/978-1-61091-512-0_5.

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Eigenbrode, Sanford D., Susan M. Capalbo, Laurie L. Houston, Jodi Johnson-Maynard, Chad Kruger i Beau Olen. "Agriculture". W Climate Change in the Northwest, 149–80. Washington, DC: Island Press/Center for Resource Economics, 2013. http://dx.doi.org/10.5822/978-1-61091-512-0_6.

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Bethel, Jeffrey, Steven Ranzoni i Susan M. Capalbo. "Human Health". W Climate Change in the Northwest, 181–206. Washington, DC: Island Press/Center for Resource Economics, 2013. http://dx.doi.org/10.5822/978-1-61091-512-0_7.

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Abdul Khalek, Md, Md Mostafizur Rahman, Md Kamruzzaman, Zubair Ahmed Shimon, M. Sayedur Rahman i Md Ayub Ali. "Modeling and Forecasting Climate Change Impact on Groundwater Fluctuations in Northwest Bangladesh". W Climate Change Management, 75–102. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-77259-8_4.

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Streszczenia konferencji na temat "Climate change- Northwest India"

ZHOU, ZUHAO, JIAJIA LIU, NING HAN, JINGYA CAI, CHONGYU XU, ZIQI YAN, YANGWEN JIA i HAO WANG. "MODELLING CLIMATE CHANGE IMPACTS ON RUNOFF IN NORTHWEST CHINA". W 38th IAHR World Congress. The International Association for Hydro-Environment Engineering and Research (IAHR), 2019. http://dx.doi.org/10.3850/38wc092019-0789.

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Hoeve, T., Fuqun Zhou i Aining Zhang. "Potential Cost Impacts for Adaptation of Building Foundations in the Northwest Territories". W 2006 IEEE EIC Climate Change Conference. IEEE, 2006. http://dx.doi.org/10.1109/eicccc.2006.277258.

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"Climate change and Environmental laws in India". W International Conference on Latest Trends in Food, Biological & Ecological Sciences. International Academy Of Arts, Science & Technology, 2014. http://dx.doi.org/10.17758/iaast.a0714023.

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Allan, Jonathan C., i Paul D. Komar. "Wave Climate Change and Coastal Erosion in the US Pacific Northwest". W Fourth International Symposium on Ocean Wave Measurement and Analysis. Reston, VA: American Society of Civil Engineers, 2002. http://dx.doi.org/10.1061/40604(273)70.

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Pali, Priyanka. "POTENTIAL FOR CLIMATE CHANGE MITIGATION THROUGH LOW-CARBON RAIL TRANSPORT IN INDIA". W International Conference on Climate Change. The International Institute of Knowledge Management-TIIKM, 2018. http://dx.doi.org/10.17501/iccc.2018.2103.

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Kubat, Ivana, Robert Gorman, Anne Collins i Garry W. Timco. "Climate Change Impact on Northern Shipping Regulations". W SNAME 7th International Conference and Exhibition on Performance of Ships and Structures in Ice. SNAME, 2006. http://dx.doi.org/10.5957/icetech-2006-108.

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The objective of this study was to find what effect climate change would have on the Zone Date System (ZDS). The paper presents an analysis of ice conditions in the Northwest Passage (NWP) shipping lanes and the access routes to the Port of Churchill in Hudson Strait. The analysis examines the existing and potential changes to ice regimes in the NWP shipping lanes due to the impact of climate change. The length of the shipping season in the NWP is analyzed for each Zone by both the ZDS and the Arctic Ice Regime Shipping System, and both systems are then compared. This paper discusses the results of the analysis.

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Patowary, S., J. Hazarika i A. K. Sarma. "Potential Impact of Climate Change on Rainfall Extremes for Urban Drainage Management". W ASCE India Conference 2017. Reston, VA: American Society of Civil Engineers, 2018. http://dx.doi.org/10.1061/9780784482025.027.

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R. Makhasana, Payal, i Geeta S. Joshi. "Assessment of Climate Change Impact using Hydro-meteorological Indicators-Rainfall, Temperature and Runoff in Mazam River Watershed, India". W International Conference on Climate Change. The International Institute of Knowledge Management - TIIKM, 2019. http://dx.doi.org/10.17501/2513258x.2019.3101.

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Singh, Shyamli, i Anugya Singh. "Climate Governance in India: A Sectoral Approach". W 2022 International Conference and Utility Exhibition on Energy, Environment and Climate Change (ICUE). IEEE, 2022. http://dx.doi.org/10.1109/icue55325.2022.10113499.

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Wardlaw, R., S. Howarth, X. Yinlong, X. Wei i Y. Yongyong. "Assessing potential climate change impacts on the Shiyang River Basin in Northwest China". W BHS 3rd International Conference. British Hydrological Society, 2010. http://dx.doi.org/10.7558/bhs.2010.ic22.

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Raporty organizacyjne na temat "Climate change- Northwest India"

D’Souza, Marcella, Arjuna Srinidhi, Shreya Banerjee, Abha Indurkar, Eshwer Kale, Larissa Stiem-Bhatia i Naman Gupta. Scaling Ecosystem-based Adaptation to Climate Change in Maharashtra, India. TMG Research gGmbH, maj 2020. http://dx.doi.org/10.35435/1.2020.1.

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Arasu, Sibi, i Kaavya Pradeep Kumar. Ways of Telling: A Handbook for Reporting on Climate Change in South India. Indian Institute for Human Settlements, 2021. http://dx.doi.org/10.24943/wthrccsi02.2021.

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Stories around climate change are not easy to tell. They are complex, technical, and develop slowly. In newsrooms where speed is king, accurate and comprehensive reporting on environmental crises often takes a hit. Scientific rigour and accuracy, sensitive representations and consistent reportage on more slow-onset events such as drought and sea-level rise are critical to build public awareness and set the agenda for more ambitious climate policies that cater to the needs of the most vulnerable.

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Takeshima, Hiroyuki, Kalyani Raghunathan i Katrina Kosec. Climate change and women’s voice and agency beyond the household: Insights from India. Washington, DC: International Food Policy Research Institute, 2022. http://dx.doi.org/10.2499/p15738coll2.136475.

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Mote, P., A. K. Snover, S. Capalbo, S. D. Eigenbrode, P. Glick, J. Littell, R. Raymondi i S. Reeder. Ch. 21: Northwest. Climate Change Impacts in the United States: The Third National Climate Assessment. Redaktorzy J. M. Melillo, Terese (T C. ). Richmond i G. W. Yohe. U.S. Global Change Research Program, 2014. http://dx.doi.org/10.7930/j04q7rwx.

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Smith, S., V. Walker i M. Burgess. Taking the chill off? Climate change in the Yukon and Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2002. http://dx.doi.org/10.4095/213590.

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MacArthur, John, Philip Mote, Jason Ideker, Miguel Figliozzi i Ming Lee. Climate Change Impact Assessment for Surface Transportation in the Pacific Northwest and Alaska. Portland State University Library, styczeń 2012. http://dx.doi.org/10.15760/trec.122.

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McNeil, Michael A., Jing Ke, Stephane de la Rue du Can, Virginie E. Letschert i James E. McMahon. Business Case for Energy Efficiency in Support of Climate Change Mitigation, Economic and Societal Benefits in India. Office of Scientific and Technical Information (OSTI), grudzień 2011. http://dx.doi.org/10.2172/1062101.

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Scott, M. J., R. D. Sands, L. W. Vail, J. C. Chatters, D. A. Neitzel i S. A. Shankle. Effects of climate change on Pacific Northwest water-related resources: Summary of preliminary findings. Office of Scientific and Technical Information (OSTI), grudzień 1993. http://dx.doi.org/10.2172/10119535.

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Sathaye, Jayant A., Kenneth Andrasko, Willy Makundi, Emilio Lebre La Rovere, N. H. Ravinandranath, Anandi Melli, Anita Rangachari i in. Concerns About Climate Change Mitigation Projects: Summary of Findings from Case Studies in Brazil, India, Mexico, and South Africa. Office of Scientific and Technical Information (OSTI), listopad 1998. http://dx.doi.org/10.2172/7284.

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Wade, John, Kelly Redmond i Peter Klingeman. The Effects of Climate Change on Energy Planning and Operations in the Pacific Northwest : Final Report. Office of Scientific and Technical Information (OSTI), wrzesień 1989. http://dx.doi.org/10.2172/6957543.

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