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backpage - Suzuki
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More than a decade ago, Suzuki developed a machine so unique that it instantly attracted a devoted following around the world. Like its namesake, the Japanese peregrine falcon, Hayabusa is famed for cutting through the air with incredible agility and performance. It combines massive thrust, unmatched maneuverability, and a silky smooth ride on city streets or the open road. Beneath its windswept design beats the legendary Suzuki Hayabusa engine. The resonating feel of pure power evokes an attitude of bold authority from both machine and rider. Through countless engineering refinements of the original design, the Hayabusa spirit has endured. Its incomparable performance delivers a fun and sporty ride at any speed, setting the bar high for rivals and defining the “Ultimate Sport Bike.” The radically original yet timeless styling also reflects the spirit of the person who owns a Hayabusa. Suzuki engineered the Hayabusa to perform like a heavyweight boxer—muscular yet surprisingly agile. While riders rarely need to call on its full punch off the line, the overabundant power and fleet-footed performance inspire confidence in everyday riding. That restrained yet refined energy is the presence that turns heads when a Hayabusa and rider pass. Hayabusa is equally at home on the highway or city streets. The low center of gravity that lets it conquer winding roads also makes Hayabusa a nimble urban predator. Plus, the Hayabusa's high-quality finish and attention to detail betray unequalled pride of craftsmanship that will become your pride of ownership. The bold design also gives it a unique aura and formidable presence not found in other bikes. The 2013 model comes newly equipped with Brembo Monobloc high-performance calipers and an Antilock Brake System. These features are sure to appeal to lone riders cruising the highway as well as touring couples.

Suzuki GSX-R1300 / Hayabusa - Fuelpak
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GSX-R1300 / HAYABUSA READ ALL INSTRUCTIONS BEFORE BEGINNING INSTALLATION TOOLS NEEDED - #1 Phillips Screwdriver - 5 mm Allen Wrench - 10 mm Socket Wrench - Less than 1 hour 08-09 Suzuki GSX-R1300 / Hayabusa Fuel Injected Models INSTALLATION INSTRUCTIONS FOR P/N 62009 INTRODUCTION: Congratulations on your purchase of the Fuelpak Fuel Management System for fuel injected Suzuki GSX-R1300 and Hayabusa motorcycles. Please take the time to read the entire instruction manual before attempting to install. DO NOT adjust the Fuelpak until you have thoroughly read the instruction manual and the unit is fully installed. If you have questions, please call (562) 921-0071. SUMMARY: To achieve the optimum performance from your application, it is recommended that you install a high performance air filter in conjunction with this unit. The Fuelpak will be installed in-line the factory injector wiring harness and the throttle position sensor. The Fuelpak will be tucked under the seat next to the ECU with the cables routing to the left side of the motorcycle. PLEASE NOTE: Fuelpak USE REQUIRES A HIGH PERFORMANCE AIR FILTER. 1. Remove the main seat and passenger seat. 2. Use a prop to hold the tank up in the trunk area.

Suzuki Hayabusa Early - Clearwater Lights

Suzuki Hayabusa 1999-2007 Glenda LED Light Kit (Dimmable) Patent Pending The Clearwater Company 2546 Mercantile Dr. Ste B Rancho Cordova, CA 95742 P:916.852.7029 F:916.852.9410 Please be sure to read our instructions thoroughly before attempting installation. Step 1: Parts List and Bike Preparation • • • Check Parts list supplied with your kit to be sure all parts are handy. Contact us at (916) 852-7029 if something is missing. Park the motorcycle on hard pavement or concrete to insure the bike will be stable during the installation. If you can mount the bike on a stand with tie-down straps, this will help secure the motorcycle Follow the manufacturers guidelines for disconnecting the battery. This is important to prevent damage to the electrical system. Note: Clearwater lights include a very high quality means of connecting to the motorcycle’s electrical system. “Posi” devices made by Posi-Products are used to securely and safely make electrical connections on the bike. You can view instructions on the proper installation of the Posi-Products at They simply screw together and mate the wires. We suggest keeping your lights on all the time, we do not furnish an “on-off” switch. It is important to be sure that the wire you use will turn off when the bike is turned off. Otherwise, you will end up with a dead battery. Nobody likes that.

Livestock and Climate Change cows, pigs, and chickens?

by Robert Goodland and Jeff Anhang undercounted or overlooked; of that subtotal, 3,000 million tons are misallocated and 22,048 million tons are entirely uncounted. When uncounted tons are added to the global inventory of atmospheric GHGs, that inventory rises from 41,755 million tons to 63,803 million tons. FAO’s 7,516 million tons of CO2e attributable to livestock then decline from 18 percent of worldwide GHGs to 11.8 percent. Let’s look at each category of uncounted or misallocated GHGs: Breathing. The FAO excludes livestock respiration from its estimate, per the following argument: Respiration by livestock is not a net source of CO2 …. Emissions from livestock respiration are part of a rapidly cycling biological system, where the plant matter consumed was itself created through the conversion of atmospheric CO2 into organic compounds. Since the emitted and absorbed quantities are considered to be equivalent, livestock respiration is not considered to be a net source under the Kyoto Protocol. Indeed, since part of the carbon consumed is stored in the live tissue of the growing animal, a growing global herd could even be considered a carbon sink. The standing stock livestock biomass increased significantly over the last decades…. This continuing growth…could be considered as a carbon sequestration process (roughly estimated at 1 or 2 million tons carbon per year). But this is a flawed way to look at the matter.

Climate Change 2014: Impacts, Adaptation, and Vulnerability ...

Human interference with the climate system is occurring,1 and climate change poses risks for human and natural systems (Figure SPM.1). The assessment of impacts, adaptation, and vulnerability in the Working Group II contribution to the IPCC’s Fifth Assessment Report (WGII AR5) evaluates how patterns of risks and potential benefits are shifting due to climate change. It considers how impacts and risks related to climate change can be reduced and managed through adaptation and mitigation. The report assesses needs, options, opportunities, constraints, resilience, limits, and other aspects associated with adaptation. Climate change involves complex interactions and changing likelihoods of diverse impacts. A focus on risk, which is new in this report, supports decision-making in the context of climate change, and complements other elements of the report. People and societies may perceive or rank risks and potential benefits differently, given diverse values and goals. Compared to past WGII reports, the WGII AR5 assesses a substantially larger knowledge base of relevant scientific, technical, and socioeconomic literature. Increased literature has facilitated comprehensive assessment across a broader set of topics and sectors, with expanded coverage of human systems, adaptation, and the ocean. See Background Box SPM.1.2 Section A of this summary characterizes observed impacts, vulnerability and exposure, and adaptive responses to date. Section B examines future risks and potential benefits. Section C considers principles for effective adaptation and the broader interactions among adaptation, mitigation, and sustainable development. Background Box SPM.2 defines central concepts, and Background Box SPM.3 introduces terms used to convey the degree of certainty in key findings. Chapter references in brackets and in footnotes indicate support for findings, figures, and tables. Figure SPM.1: Illustration of the core concepts of the WGII AR5. Risk of climate-related impacts results from the interaction of climate-related hazards (including hazardous events and trends) with the vulnerability and exposure of human and natural systems. Changes in both the climate system (left) and socioeconomic processes including adaptation and mitigation (right) are drivers of hazards, exposure, and vulnerability. [19.2, Figure 19-1]...

IPCC AR4 Chapter 10 - Global Climate Projections

The future climate change results assessed in this chapter are based on a hierarchy of models, ranging from AtmosphereOcean General Circulation Models (AOGCMs) and Earth System Models of Intermediate Complexity (EMICs) to Simple Climate Models (SCMs). These models are forced with concentrations of greenhouse gases and other constituents derived from various emissions scenarios ranging from nonmitigation scenarios to idealised long-term scenarios. In general, we assess non-mitigated projections of future climate change at scales from global to hundreds of kilometres. Further assessments of regional and local climate changes are provided in Chapter 11. Due to an unprecedented, joint effort by many modelling groups worldwide, climate change projections are now based on multi-model means, differences between models can be assessed quantitatively and in some instances, estimates of the probability of change of important climate system parameters complement expert judgement. New results corroborate those given in the Third Assessment Report (TAR). Continued greenhouse gas emissions at or above current rates will cause further warming and induce many changes in the global climate system during the 21st century that would very likely be larger than those observed during the 20th century. Mean Temperature All models assessed here, for all the non-mitigation scenarios considered, project increases in global mean surface air temperature (SAT) continuing over the 21st century, driven mainly by increases in anthropogenic greenhouse gas concentrations, with the warming proportional to the associated radiative forcing. There is close agreement of globally averaged SAT multi-model mean warming for the early 21st century for concentrations derived from the three non-mitigated IPCC Special Report on Emission Scenarios (SRES: B1, A1B and A2) scenarios (including only anthropogenic forcing) run by the AOGCMs (warming averaged for 2011 to 2030 compared to 1980 to 1999 is between +0.64°C and +0.69°C, with a range of only 0.05°C). Thus, this warming rate is affected little by different scenario assumptions or different model sensitivities, and is consistent with that observed for the past few decades (see Chapter 3).

The Politicization of Climate Change and Polarization in ... - EPSCoR

Riley E. Dunlap Oklahoma State University We examine political polarization over climate change within the American public by analyzing data from 10 nationally representative Gallup Polls between 2001 and 2010. We find that liberals and Democrats are more likely to report beliefs consistent with the scientific consensus and express personal concern about global warming than are conservatives and Republicans. Further, the effects of educational attainment and self-reported understanding on global warming beliefs and concern are positive for liberals and Democrats, but are weaker or negative for conservatives and Republicans. Last, significant ideological and partisan polarization has occurred on the issue of climate change over the past decade. The Western experience of modernity—especially technological development, economic growth, material prosperity, urbanization, and democracy—has been built upon industrial capitalism, an economic system predicated on the accelerating extraction and consumption of fossil fuels for energy (Clark and York 2005). A major unintended consequence of the use of fossil fuels is anthropogenic global warming or climate change.1 Recognizing and responding to climate change, arguably the most challenging social problem of the modern era (Giddens 2009), thus poses a fundamental critique of continued modernization processes around the world (Antonio 2009). For two decades, European-based reflexive modernization theorists (e.g., Beck, Giddens, and Lash 1994; Mol 1996) have argued that forces of reflexivity, particularly science and environmentalism, compel us to confront threats to societal persistence such as climate change.2 In contrast, stimulated by the United States’s long-term, laggard response to climate change, a growing number of scholars have begun calling attention to forces of “anti-reflexivity” (McCright and Dunlap 2010)—particularly the industrial sector and the conservative movement—that defend the industrial capitalist order from critique by denying the significance of problems such as climate change (also see, e.g., *Direct all correspondence to Aaron M. McCright, Lyman Briggs College, Michigan State University, E-185 Holmes Hall, East Lansing, MI 48825-1107; e-mail: The Sociological Quarterly 52 (2011) 155–194 © 2011 Midwest Sociological Society

Detection and Attribution of Climate Change: from Global to Regional

Atmospheric Temperatures More than half of the observed increase in global mean surface temperature (GMST) from 1951 to 2010 is very likely1 due to the observed anthropogenic increase in greenhouse gas (GHG) concentrations. The consistency of observed and modeled changes across the climate system, including warming of the atmosphere and ocean, sea level rise, ocean acidification and changes in the water cycle, the cryosphere and climate extremes points to a large-scale warming resulting primarily from anthropogenic increases in GHG concentrations. Solar forcing is the only known natural forcing acting to warm the climate over this period but it has increased much less than GHG forcing, and the observed pattern of long-term tropospheric warming and stratospheric cooling is not consistent with the expected response to solar irradiance variations. The Atlantic Multi-decadal Oscillation (AMO) could be a confounding influence but studies that find a significant role for the AMO show that this does not project strongly onto 1951–2010 temperature trends. {10.3.1, Table 10.1} It is extremely likely that human activities caused more than half of the observed increase in GMST from 1951 to 2010. This assessment is supported by robust evidence from multiple studies using different methods. Observational uncertainty has been explored much more thoroughly than previously and the assessment now considers observations from the first decade of the 21st century and simulations from a new generation of climate models whose ability to simulate historical climate has improved in many respects relative to the previous generation of models considered in AR4. Uncertainties in forcings and in climate models’ temperature responses to individual forcings and difficulty in distinguishing the patterns of temperature response due to GHGs and other anthropogenic forcings prevent a more precise quantification of the temperature changes attributable to GHGs. {9.4.1, 9.5.3, 10.3.1, Figure 10.5, Table 10.1} GHGs contributed a global mean surface warming likely to be between 0.5°C and 1.3°C over the period 1951–2010, with the contributions from other anthropogenic forcings likely to be between –0.6°C and 0.1°C, from natural forcings likely to be between –0.1°C and 0.1°C, and from internal variability likely to be between –0.1°C and 0.1°C. Together these assessed contributions are consistent with the observed warming of approximately 0.6°C over this period. {10.3.1, Figure 10.5} It is virtually certain that internal variability alone cannot account for the observed global warming since 1951. The observed global-scale warming since 1951 is large compared to climate model estimates of internal variability on 60-year time scales.

SBMPTN 2013 Biologi - Bisa Kimia

Doc. Name: SBMPTN2013BIO999 Doc. Version : 2013-10 | 01. Contoh keberadaan satwa pada suatu habitat yang dijaga dengan baik sebagai upaya pelestarian ex situ adalah… (A) Orang utan di hutan Kalimantan. (B) Cendrawasih di hutan Papua. (C) Rusa di Kebun Raya Bogor. (D) Pesut diSungai Mahakam. (E) Anoa di Pulau Sulawesi 02. Komunitas mikroba yang melekat pada suatu substrat/benda sehingga dapat merusak substrat/benda tersebut disebut… (A) Biodegradator. (B) Bioaktivator. (C) Biokatalis. (D) Biodeposit. (E) Biofilm. 03. Bagian sistem pencernaan yang berperan dalam memecah polipeptida menjadi oligopeptida adalah… (A) Duodenum. (B) Usus besar. (C) Lambung. (D) Jejunum. (E) Ileum. 04. Asam absisat melindungi tanaman yang mengalami kekurangan air melalui mekanisme… (A) Peningkatan pembentukan kutikula. (B) Penurunan tekanan turgor sel penjaga. (C) Peningkatan kecepatan pembelahan sel. (D) Penurunan kecepatan pembentangan sel. (E) Penghambatan pemanjangan sel epidermis. halaman 1 05. Pernyataan yang salah mengenai fotofosforilisasi siklik dan non siklik adalah… (A) Pada fotofosforilisasi non siklik sumber elektron yang memasuki Fotosistem II adalah molekul air, pada fotofosforilisasi siklik, sumber dari elektron adalah Fotosistem I. (B) Pada fotofosforilisasi non siklik penerima elktron terakhir adalah NADP, pada fotofosforilisasi siklik, penerima elektron terakhir adalah Fotosistem I. (C) Hasil dari fotofosforilisasi non siklik adalah ATP, NADPH, dan O2, sedangkan hasil dari fotofosforilisasi siklikhanya ATP. (D) Fotofosforilisasi non siklik melibatkan Fotosistem I dan II, fotofosforilisasi siklik hanya melibatkan Fotosistem II. 06. Perhatikan diagram saluran kreb berikut! Tahap dimana berlangsung hidrasi adalah (A) 1 dan 4 (B) 1 dan 5 (C) 2 dan 6 (D) 3 dan 7 (E) 3 dan 8 Kunci dan pembahasan soal ini bisa dilihat di dengan memasukkan kode 3117 ke menu search. Copyright © 2013 Zenius Education SBMPTN 2013 Biologi, Kode Soal doc. name: SBMPTN2013BIO999 halaman 2 doc. version : 2013-10 | 07. Perhatikan gambar tahapan mitosis berikut! 10. Grafik berikut menunjukan kinerja insulin sintetis. Tahap telofase, metaphase, anaphase dan profasen ditunjukan oleh urutan angka…

SNMPTN 2012 - Siap Belajar
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SELEKSI NASIONAL MASUK PERGURUAN TINGGI NEGERI Disertai TRIK SUPERKILAT dan LOGIKA PRAKTIS Fisika IPA Disusun Oleh : Pak Anang Kumpulan SMART SOLUTION dan TRIK SUPERKILAT Pembahasan Soal SNMPTN 2012 Fisika IPA Kode Soal 634 By Pak Anang ( 16. Gerak sebuah benda dijelaskan oleh grafik hubungan antara kecepatan dan waktu seperti ditunjukkan gambar di bawah ini. TRIK SUPERKILAT: Jarak adalah luas daerah pada grafik 𝑣 − 𝑡: 𝑣(m/s) 4 −5 8 𝑡(s) −10 𝑠 = Luas segiempat + Luas trapesium 1 = (𝑝 × ℓ) + 𝑡(𝑎 + 𝑏) 2 1 = (5 × 4) + 4(5 + 10) 2 = 20 + 30 = 50 m Jarak yang ditempuh oleh benda hingga detik ke-8 adalah .... A. 60 m B. 50 m C. 45 m D. 40 m E. 30 m Penyelesaian: Ingat! Pada gerak GLB, jarak dirumuskan dengan: 𝑠 = 𝑣𝑡 Pada gerak GLBB, jarak dirumuskan dengan: 𝑠 = 𝑣0 𝑡 + 1 2 𝑎𝑡 2 Dari grafik kita bisa melihat bahwa benda bergerak mundur secara GLB pada detik ke-0 hingga detik ke-4. Sehingga, jarak yang ditempuh benda saat bergerak GLB adalah: 𝑠1 = 𝑣𝑡 = (−5) × 4 = −20 m Lalu benda kembali bergerak mundur secara GLBB pada detik ke-4 hingga detik ke-8, benda mengalami perlambatan sebesar: ∆𝑣 −10 − (−5) −5 = = = −1,25 ms −2 ∆𝑡 8−4 4 Sehingga jarak yang ditempuh benda saat bergerak GLBB adalah: 𝑎= 𝑠2 = 𝑣0 𝑡 + 1 2 1 𝑎𝑡 = ((−5) × 4) + ( × (−1,25) × (4)2 ) = (−20) + (−10) = −30 m 2 2 Jadi total jarak yang ditempuh benda adalah: 𝑠 = 𝑠1 + 𝑠2 = (−20) + (−30) = −50 m (tanda negatif menyatakan benda bergerak mundur) Bimbel SBMPTN 2013 Fisika by Pak Anang ( Halaman 1 17. Kedua ujung sebuah pegas yang memiliki tetapan pegas 50 N/m ditarik masing-masing dengan gaya sebesar 10 N yang saling berlawanan. Pertambahan panjang pegas tersebut adalah .... A. 0,0 m TRIK SUPERKILAT: B. 0,1 m Meskipun pegas menerima dua gaya yang sama besar dan C. 0,2 m berlawanan arah, bukan berarti pegas akan tambah panjang dua kali lipat. Karena kedua gaya tersebut adalah gaya aksi reaksi. D. 0,3 m Sehingga total pertambahan panjang pegas adalah 2𝑥. E. 0,4 m 𝐹 10 𝑥= Penyelesaian: 𝑘 = 50 = 0,2 m Ingat! Pada pegas berlaku: 𝐹 = 𝑘𝑥 Pada soal diketahui: 𝑘 = 50 N/m 𝐹1 = 10 𝑁 𝐹2 = −10 𝑁 (tanda negatif karena arah berlawanan dengan 𝐹1 ) Sehingga pertambahan panjang oleh sebuah gaya 𝐹 = 10 N pada pegas adalah: 𝐹 = 𝑘𝑥 ⇒ 𝑥 = 𝐹 10 = = 0,2 m 𝑘 50 𝑭𝟐 𝑭𝟏 𝑭𝟏 𝑭𝟐 𝒙 Jadi, meskipun ada dua gaya yang sama besar dan berlawanan pada pegas, namun dalam hal ini kedua gaya adalah pasangan gaya aksi-reaksi, sehingga gaya yang beriteraksi pada pegas sebenarnya hanyalah gaya sebesar 10 N saja. Jadi pertambahan panjang pegas adalah:...