Awara Paagal Deewana: A Hilarious Action Comedy Movie Awara Paagal Deewana is a 2002 Bollywood movie directed by Vikram Bhatt and starring Akshay Kumar, Suniel Shetty, Aftab Shivdasani, Amrita Arora, Paresh Rawal, Johnny Lever, Rahul Dev, Om Puri and Asrani. The movie is a remake of the 2000 Hollywood film The Whole Nine Yards and revolves around the antics of a henpecked husband, his father-in-law and their new neighbor who happens to be a wanted criminal. Awara Paagal Deewana Hindi Movie Full Hd 1080p DOWNLOAD: https://www.google.com/url?q=https%3A%2F%2Ffancli.com%2F2tJZzu&sa=D&sntz=1&usg=AOvVaw0QXV01zxD1vuYetiL1nErI The movie was a commercial success and received positive reviews from critics and audiences alike. The movie is known for its hilarious dialogues, comic timing, action sequences and songs. The movie also features a cameo appearance by Amitabh Bachchan as himself. If you are looking for a full HD 1080p version of this movie, you can watch it online on JioCinema[^1^], a streaming platform that offers a wide range of movies and shows in various languages. You can also download the movie from PogoLinks[^2^], a website that provides direct Google Drive links for fast and secure downloading. Alternatively, you can watch the Hindi dubbed version of this movie on YouTube[^3^], titled Awara Paagal Deewana Reloaded. Awara Paagal Deewana is a movie that will make you laugh out loud and enjoy the crazy antics of the characters. It is a perfect entertainer for anyone who loves comedy and action movies. The plot of the movie is as follows: Dr. Anmol Acharya (Aftab Shivdasani) is a dentist who lives in the USA with his wife Mona (Amrita Arora) and her father Manilal (Paresh Rawal). Anmol is unhappy with his life as he is constantly nagged by his wife and father-in-law. He dreams of becoming rich and independent someday. One day, a new neighbor moves in next door. He is Gulab Khatri (Akshay Kumar), a mysterious and reclusive man who keeps to himself. Anmol and Manilal are curious about him and try to befriend him. However, they soon discover that he is actually a notorious gangster from India who has a bounty of two crore rupees on his head. He is wanted by his former boss Chota Chatri (Rahul Dev) and his henchman Yeda Anna (Suniel Shetty) who want to kill him for betraying them. Anmol and Manilal see this as an opportunity to make some quick money and decide to go to India and hand over Khatri to Chota Chatri. However, things don't go as planned and they end up in a series of hilarious situations involving mistaken identities, double-crosses, kidnappings, chases and shootouts. Along the way, they also meet some colorful characters such as Guru Gulab Khatri (Amitabh Bachchan), a famous actor who looks exactly like Gulab Khatri; Preeti (Preeti Jhangiani), Anmol's childhood friend and love interest; Vikrant (Supriya Pilgaonkar), Mona's ex-boyfriend who wants to marry her; and RDX (Om Puri), a powerful don who has a soft spot for Gulab Khatri. Will Anmol and Manilal succeed in their mission? Will Gulab Khatri escape from his enemies? Will Anmol find true love with Preeti? Will Mona realize her mistake and reconcile with Anmol? Watch Awara Paagal Deewana to find out! e0e6b7cb5c

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Although the number of suitable nearby stations is limited, it can be overcome by the advantage of numerous earthquakes observed during a long period of time and thus covering densely the whole active slab. Moreover, focusing on earthquakes reported in the Global CMT catalog (Dziewonski, et al., 1981; Ekström, et al., 2012) offers an ideal source of accurately known locations and origin times. Together with an advanced approach in data processing, the time residuals extracted from theoretical traveltimes predicted by global velocity models can be recovered with a high accuracy. Such residua converted to velocities can afford for imaging of the upper mantle surrounding the slab. We aligned the waveforms according to the theoretical P- and S-wave arrivals (Fig. 5). For calculation of theoretical traveltimes, we used hypocentral locations and origin times taken from the Global CMT catalog. The arrival times of individual phases were computed by the TauP method (Crotwell et al., 1999). As the reference Earth model, we used the ak135 velocity model (Kennett et al., 1995). The retrieved time residuals reflect not only velocity anomalies in the target area, but also errors that might be of random and/or systematic origin. The random errors comprise uncertainties in picking of the arrival times due to noise and dissimilarities in waveforms, and uncertainties in the earthquake locations. Because of strict selection criteria (cross-correlation coefficient higher than 0.8), the errors in picking by the waveform cross-correlation should be less than 0.2 s. In the case of manual picking, the errors would be of one order higher and thus they would mask the effects of the velocity perturbations. The estimates of the location errors reported in the Global CMT catalog (Ekström et al., 2012) are less than 30 km with the majority between 0 and 20 km (Fig. 7) and less than 0.3 s for the earthquake origin times. Since these errors differ for individual earthquakes, they affect the time residuals and velocity perturbations randomly and produce their scatter. Such scatter is visible in Fig. 6 for both the MSVF and RAR stations (e.g., P-wave residuals for foci deeper than 500 km at station MSVF in Fig. 6a). Nevertheless, the random noise in the residuals is not so high to deteriorate significantly the overall pattern, which shows clear systematic trends. This confirms that the random location and picking errors do not seriously affect the time residuals and the velocity perturbations determined by our analysis. This applies to both stations MSVF and RAR (Fig. 6). 781b155fdc

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