<?xml version="1.0" encoding="UTF-8" standalone="no"?><?xml-stylesheet href="http://www.blogger.com/styles/atom.css" type="text/css"?><rss xmlns:itunes="http://www.itunes.com/dtds/podcast-1.0.dtd" version="2.0"><channel><title>info dunia</title><description></description><managingEditor>noreply@blogger.com (puwokertoinfo)</managingEditor><pubDate>Thu, 26 Sep 2024 20:47:38 -0700</pubDate><generator>Blogger http://www.blogger.com</generator><openSearch:totalResults xmlns:openSearch="http://a9.com/-/spec/opensearchrss/1.0/">5</openSearch:totalResults><openSearch:startIndex xmlns:openSearch="http://a9.com/-/spec/opensearchrss/1.0/">1</openSearch:startIndex><openSearch:itemsPerPage xmlns:openSearch="http://a9.com/-/spec/opensearchrss/1.0/">25</openSearch:itemsPerPage><link>http://top-tips-today.blogspot.com/</link><language>en-us</language><itunes:explicit>no</itunes:explicit><itunes:subtitle/><itunes:owner><itunes:email>noreply@blogger.com</itunes:email></itunes:owner><item><title>Asian markets</title><link>http://top-tips-today.blogspot.com/2009/03/asian-markets.html</link><author>noreply@blogger.com (puwokertoinfo)</author><pubDate>Fri, 13 Mar 2009 20:14:00 -0700</pubDate><guid isPermaLink="false">tag:blogger.com,1999:blog-4583422652989818656.post-5503526287590221497</guid><description>&lt;!-- node template --&gt;   &lt;h1&gt;Asian markets extend global rally on Citi news&lt;/h1&gt;   Asian stock markets surged Tuesday, with Japan's key index jumping nearly 5 percent, after Wall Street staged a massive rally as news that Citigroup is turning a profit buoyed hopes the stricken financial sector can recover.&lt;br /&gt;&lt;br /&gt;The region's lurch higher, led partly by financial shares, was a welcome reprieve from the depressing declines in global equities over the last few weeks.&lt;br /&gt;&lt;br /&gt;But analysts said the relief was likely to be temporary as stocks, in the throes of the worst bear market in years, continue to grind toward a new bottom in the coming months amid the worsening outlook for the world economy. Another sharp drop in Chinese exports last month was just the latest grim reminder of how severe the global downturn is.&lt;br /&gt;&lt;br /&gt;"What you've seen today is mostly a technical bounce in markets after falling steeply recently, and I don't think this rally can be sustained," said Arjuna Mahendran, the Singapore-based head of Asian investment strategy for HSBC Private Bank, which manages some US$494 billion in assets. "It's still far too early to predict that the global recession is over ... The fundamentals are simply not in place."&lt;br /&gt;&lt;br /&gt;The catalyst for the rally on Wall Street was a letter from Citigroup Chief Executive Vikram Pandit to employees saying the bank had operated at a profit for the first two months of this year, logging its best performance since the third quarter of 2007, the last time it booked a quarterly profit.&lt;br /&gt;&lt;br /&gt;Investors, desperate for any positive signs about the ailing financial system, cheered the news about the banking giant, which has lost so much money the federal government has been forced to extend billions in aid and take a 36 percent stake.&lt;br /&gt;&lt;br /&gt;Japan's Nikkei 225 stock average shot up 321.14 points, or 4.6 percent, to 7,376.12, rebounding from a 26-year closing low hit this week. Hong Kong's Hang Seng leaped 332.56 points, or 2.8 percent, to 12,026.61.&lt;br /&gt;&lt;br /&gt;Elsewhere, South Korea's Kospi rose 35.31, or 3.2 percent, to 1,127.51. Benchmarks in Australia, Singapore and Taiwan were up 1.9 percent.&lt;br /&gt;&lt;br /&gt;Banking shares were especially strong, with leading Japanese bank Mitsubishi UFJ Financial Group Inc. gaining 4 percent. HSBC, which like Citi gave reassurances this week that it was performing better than expected so far this year, advanced 6 percent in Hong Kong, continuing its recovery form a 24 percent plunge on Monday.&lt;br /&gt;&lt;br /&gt;The upbeat mood, though, belied more evidence that Asian countries were still suffering from the drought in Western demand that drives their export-reliant economies.&lt;br /&gt;&lt;br /&gt;In China, exports plunged 25.7 percent last month as overseas appetites for goods made in the world's third-largest economy continued to deteriorate. Imports also fell. A string of monthly export declines is undermining hopes among many investors that China can boost its economy, at least in the near term, with a 4 trillion ($586 billion) stimulus package.&lt;br /&gt;&lt;br /&gt;Also in Asia, Japanese machinery orders, an indicator of how much the country's companies are spending, fell 3.2 percent in January, though were still better than expected.&lt;br /&gt;&lt;br /&gt;In the U.S., Federal Reserve chairman Ben Bernanke warned the U.S. recession wouldn't end this year unless the government bailout of banks succeeded and financial markets were restored to working order.&lt;br /&gt;&lt;br /&gt;On Tuesday, Wall Street posted its best performance of the year, with the Dow Jones industrials surging 379 points, or about 5.8 percent, to 6,926.49. The broader Standard &amp;amp; Poor's 500 index advanced 43.07 points, 6.4 percent, to 719.6.&lt;br /&gt;&lt;br /&gt;Stock futures pointed to modest gains on Wall Street Wednesday. Dow futures rose 46, or 0.7 percent, to 6,933 and S&amp;amp;P 500 futures advanced 4.5, or 0.6 percent, to 720.50.&lt;br /&gt;&lt;br /&gt;Oil prices were steady in Asian trade, with light, sweet crude for April delivery up 5 cents at $45.76 a barrel on the New York Mercantile Exchange. The contract fell $1.36 to settle at $45.71 a barrel overnight.&lt;br /&gt;&lt;br /&gt;The dollar weakened to 98.54 yen from 98.80 yen late Tuesday. The euro dropped to $1.2629 from $1.2702.</description><thr:total xmlns:thr="http://purl.org/syndication/thread/1.0">0</thr:total></item><item><title>indo today</title><link>http://top-tips-today.blogspot.com/2009/03/indo-today.html</link><author>noreply@blogger.com (puwokertoinfo)</author><pubDate>Thu, 12 Mar 2009 20:14:00 -0700</pubDate><guid isPermaLink="false">tag:blogger.com,1999:blog-4583422652989818656.post-3036674939431418797</guid><description>&lt;span style="font-size:100%;"&gt;Asking for NGO’s accountability may sound like a harsh question,            but that is in fact the underlying issue for all the debates related            to the evolving relationship between the UN and NGOs over the decades.           &lt;br /&gt;         &lt;br /&gt;          Substantial efforts have been made to address this question, even at            the highest level of global governance. A Panel of Eminent Persons on            UN-Civil Society relations was established by the UN Secretary General            in 2003 to make report and recommendations on the issue. At the 2005            Summit, World Leaders welcomed the positive contributions of civil society            organizations, including NGOs, to the work of the UN. They also encouraged            continued dialogue between civil society and Member States. &lt;/span&gt;         &lt;p align="justify"&gt;&lt;span style="font-size:100%;"&gt;Yet, the question continues to raise            anxieties for many. &lt;/span&gt;&lt;/p&gt;         &lt;p align="justify"&gt;&lt;span style="font-size:100%;"&gt;There is a general consensus on the            need for continued dialogue and interaction between Member States and            NGOs. At the same time, there are different expectations and preferences            on how to manage and develop it further. &lt;/span&gt;&lt;/p&gt;         &lt;p align="justify"&gt;&lt;span style="font-size:100%;"&gt;Last year, together with H.E. Ambassador            Johan L. Lovald of Norway, the writer had the opportunity to act as            a personal advisor of the President of the 60th General Assembly on            the relationship between Member States and civil society, including            NGOs. Discussions were held with representatives of Member States, NGOs            and related UN agencies, regarding current practices of NGO engagement            in the work of the UN and future expectations. &lt;/span&gt;&lt;/p&gt;         &lt;p align="justify"&gt;&lt;span style="font-size:100%;"&gt;While confirming the existence of clear            differences on various issues between Member States and NGOs, it was            heartening to note that there was sufficient common ground to develop            more meaningful, constructive and workable partnerships and interaction            between both sides.&lt;/span&gt;&lt;/p&gt;         &lt;p align="justify"&gt;&lt;span style="font-size:100%;"&gt;Both agreed on the fundamentality of            the intergovernmental nature of the United Nations. Both also agreed            that further measures for increased interaction could be envisaged.            Among the important measures identified was to address the so-called            “confidence deficit”. &lt;/span&gt;&lt;/p&gt;         &lt;p align="justify"&gt;&lt;span style="font-size:100%;"&gt;It was clear that a certain “confidence            deficit” existed at the heart of the relationship between Member            States and NGOs. This has raised a question pertaining to the NGO accountability,            especially in connection with their involvement in the work of the United            Nations. &lt;/span&gt;&lt;/p&gt;         &lt;p align="justify"&gt;&lt;span style="font-size:100%;"&gt;This is particularly relevant in light            of the fact that NGOs have greatly proliferated and become more visible            while remaining relatively unregulated in many parts of the world. A            lack of international standard of NGO accountability has allowed far            less credible organizations to undermine the effectiveness of credible            NGOs. There is a legitimate concern over the question of NGO accountability,            one underlying factor behind the confidence deficit. &lt;/span&gt;&lt;/p&gt;         &lt;p align="justify"&gt;&lt;span style="font-size:100%;"&gt;Member States generally appear to be            open to increased consultation with NGOs as long as there are clear            parameters that are understood and respected by all. NGOs are valued            for their expertise in a variety of areas, their role as partners in            implementing various development programs, and their capacity to provide            early warning in cases of potential conflicts.&lt;/span&gt;&lt;/p&gt;         &lt;p align="justify"&gt;&lt;span style="font-size:100%;"&gt;Many NGOs themselves also emphasized            the importance of accountability and wished to exercise due diligence            for NGOs attending UN meetings. Accountability was viewed to be integral            to establishing meaningful dialogue between Member States and NGOs.&lt;/span&gt;&lt;/p&gt;         &lt;p align="justify"&gt;&lt;span style="font-size:100%;"&gt;Questioning NGO accountability should            not be viewed as an unfriendly attempt to disengage. Instead, it reflects            growing recognition of the increased role of civil society, including            NGOs, in shaping public policy across the world. &lt;/span&gt;&lt;/p&gt;         &lt;p align="justify"&gt;&lt;span style="font-size:100%;"&gt;Such role needs to be accompanied by            accountability, however.&lt;/span&gt;&lt;/p&gt;         &lt;p align="justify"&gt;&lt;span style="font-size:100%;"&gt;The notion of NGO accountability needs            to be defined and developed. This is not an easy task because of the            multiplicity of actors with whom the NGOs engage. Yet, several areas            certainly need to be addressed in this regard.&lt;/span&gt;&lt;/p&gt;         &lt;p align="justify"&gt;&lt;span style="font-size:100%;"&gt;There should be a recognized standards            by the NGO community for their integrity and performance. The participation            in the work of the UN should be granted to organizations that truly            have expertise in the area being discussed.&lt;/span&gt;&lt;/p&gt;         &lt;p align="justify"&gt;&lt;span style="font-size:100%;"&gt;The idea of a code of conduct for NGOs            is also worth further exploration. The code of conduct can be an instrument            to ensure that NGOs commit themselves to the aims of the Charter and            act in a manner that respects the intergovernmental character of the            UN. &lt;/span&gt;&lt;/p&gt;         &lt;p align="justify"&gt;&lt;span style="font-size:100%;"&gt;There should be a level playing field            for NGOs involvement, in that the NGOs attending UN meetings are truly            representative of the world’s population. This brings up the crucial            issue of the participation of NGOs from developing countries. &lt;/span&gt;&lt;/p&gt;         &lt;p align="justify"&gt;&lt;span style="font-size:100%;"&gt;As of 2005, approximately 67% of all            NGOs in consultative status with Economic and Social Council (ECOSOC)            came from developed countries, which only constitute 20% of the world’s            countries. Understandably, developing countries sometimes view NGOs            involvement as another channel to push the “Northern agenda”.            &lt;/span&gt;&lt;/p&gt;         &lt;p align="justify"&gt;&lt;span style="font-size:100%;"&gt;Several initiatives have been identified            to address this imbalance, including optimizing the use of information            and communication technology and establishing a trust fund to provide            financial assistance to NGO representatives from developing countries.            &lt;/span&gt;&lt;/p&gt;         &lt;p align="justify"&gt;&lt;span style="font-size:100%;"&gt;These are only some of the areas that            can be elaborated further. This is a healthy process towards a realistic            framework for balancing interests and respecting the different roles            of Member States and NGOs within the UN process. This is also a positive            sign of the growing maturity of the international community in welcoming            the role and contributions of civil society, including the NGOs.&lt;br /&gt;         &lt;br /&gt;          In the evolving relationship between the UN and NGOs, NGOs may not be            able to claim to be the representative of all the peoples, but they            can definitely give voice to a wide range of opinion which emerges in            various segments of society. &lt;/span&gt;&lt;/p&gt;</description><thr:total xmlns:thr="http://purl.org/syndication/thread/1.0">0</thr:total></item><item><title>Indonesia Today: A Road to Democracy</title><link>http://top-tips-today.blogspot.com/2009/03/indonesia-today-road-to-democracy.html</link><author>noreply@blogger.com (puwokertoinfo)</author><pubDate>Tue, 10 Mar 2009 20:08:00 -0700</pubDate><guid isPermaLink="false">tag:blogger.com,1999:blog-4583422652989818656.post-8863923721898746618</guid><description>&lt;p&gt;President Abdurrahman Wahid (popularly known as Gus Dur),                          whose term of office was supposed to run until 2004, lost                          his presidency when the People's Consultative Assembly                          (MPR) revoked its mandate and appointed Vice President                          Megawati Soekarnoputri as a new president.                       &lt;/p&gt;&lt;p&gt;In a special session on July 23, 2001, ahead of the scheduled                          date of August 1, 2001, the Assembly revoked its mandate                          to Wahid on the grounds that he had exceeded his authority,                          particularly by issuing a decree suspending the Assembly                          and the House of Representatives (DPR).&lt;/p&gt;                       &lt;p&gt;With the appointment of Megawati Soekarnoputri, chairman                          of the Indonesian Democratic Party for Struggle (PDIP                          - the party which won the 1999 election), Indonesia now                          has a president elected by democratic and constitutional                          means.&lt;/p&gt;                       &lt;p&gt;Three days after the appointment of Megawati as a new                          president, Hamzah Haz, chairman of the Indonesian United                          Party (PPP), was elected the country's ninth vice president.                          Hamzah garnered a majority of votes in the third round                          of the vice presidential ballot. The appointment of Hamzah                          as vice president is expected to bring renewed hope for                          peace with a call for political parties to come together                          to support President Megawati Soekarnoputri's government.&lt;/p&gt;                       &lt;p&gt;The new national leadership duo of President Megawati                          and Vice President Hamzah Haz is expected to defuse the                          political and economic turmoil that has plagued the country                          for the past three years. &lt;/p&gt;                       &lt;p&gt;Megawati will lead Indonesia until 2004, after which                          Indonesia will have another general election. &lt;/p&gt;                       &lt;p&gt;The world's largest archipelago is still in the process                          of democratisation despite the ongoing economic crisis.                          By definition, democracy means that all citizens can exercise                          their right to speak freely and to vote in free elections,                          rights that have previously not been widely exercised                          in this country. Indonesia is experiencing a positive                          trend in this regard, following the emergence of the reform                          movement spearheaded by university students in May 1998.&lt;/p&gt;                       &lt;p&gt;It all started when students of almost all universities                          in Indonesia held a series of rallies demanding reforms                          in the government, which led to the resignation of Soeharto                          in May 21, 1998. The first democratic election on June                          7, 1999 was seen by many as a landmark for the country                          after more than three decades of authoritarian rule. Indonesia                          then held a presidential election in October 1999 that                          brought Abdurrahman Wahid to the presidency.&lt;/p&gt;                       &lt;p&gt;The road to democracy is long in such large and complex                          country, but we are well on the way and determined to                          reach our goals.&lt;/p&gt;                       &lt;p&gt;&lt;br /&gt;                      &lt;/p&gt;</description><thr:total xmlns:thr="http://purl.org/syndication/thread/1.0">0</thr:total></item><item><title>Solar variation to global warming</title><link>http://top-tips-today.blogspot.com/2009/03/solar-variation-to-global-warming.html</link><category>top</category><author>noreply@blogger.com (puwokertoinfo)</author><pubDate>Mon, 9 Mar 2009 20:07:00 -0700</pubDate><guid isPermaLink="false">tag:blogger.com,1999:blog-4583422652989818656.post-8285533359066084135</guid><description>   	&lt;meta http-equiv="CONTENT-TYPE" content="text/html; charset=utf-8"&gt; 	&lt;title&gt;&lt;/title&gt; 	&lt;meta name="GENERATOR" content="OpenOffice.org 2.4  (Linux)"&gt; 	&lt;style type="text/css"&gt; 	&lt;!-- 		@page { size: 8.5in 11in; margin: 0.79in } 		P { margin-bottom: 0.08in } 		H3 { margin-bottom: 0.08in } 	--&gt; 	&lt;/style&gt;  &lt;p style="margin-bottom: 0.2in;"&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt; &lt;p&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;One alternative &lt;a href="http://en.wikipedia.org/wiki/Hypothesis"&gt;hypothesis&lt;/a&gt; to the consensus view that &lt;a href="http://en.wikipedia.org/wiki/Anthropogenic"&gt;anthropogenic&lt;/a&gt; forcing has caused most of the recent temperature increase is that recent warming may be the result of variations in solar activity.&lt;/span&gt;&lt;/p&gt; &lt;p&gt;&lt;a name="cite_ref-29"&gt;&lt;/a&gt;&lt;a name="cite_ref-30"&gt;&lt;/a&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;A paper by Peter Stott and colleagues suggests that climate models overestimate the relative effect of greenhouse gases compared to solar forcing; they also suggest that the cooling effects of volcanic dust and sulfate aerosols have been underestimated.&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-29"&gt;[30]&lt;/a&gt; They nevertheless conclude that even with an enhanced climate sensitivity to solar forcing, most of the warming since the mid-20th century is likely attributable to the increases in greenhouse gases. Another paper suggests that the Sun may have contributed about 45–50 percent of the increase in the average global surface temperature over the period 1900–2000, and about 25–35 percent between 1980 and 2000.&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-30"&gt;[31]&lt;/a&gt;&lt;/span&gt;&lt;/p&gt; &lt;p style="margin-bottom: 0in;"&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;Solar variation over the last thirty years.&lt;/span&gt;&lt;/p&gt; &lt;p&gt;&lt;a name="cite_ref-31"&gt;&lt;/a&gt;&lt;a name="cite_ref-32"&gt;&lt;/a&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;A different hypothesis is that variations in &lt;a href="http://en.wikipedia.org/wiki/Solar_variation"&gt;solar output&lt;/a&gt;, possibly amplified by cloud seeding via &lt;a href="http://en.wikipedia.org/wiki/Galactic_cosmic_ray"&gt;galactic cosmic rays&lt;/a&gt;, may have contributed to recent warming.&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-31"&gt;[32]&lt;/a&gt; It suggests magnetic activity of the sun is a crucial factor which deflects cosmic rays that may influence the generation of cloud condensation nuclei and thereby affect the climate.&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-32"&gt;[33]&lt;/a&gt;&lt;/span&gt;&lt;/p&gt; &lt;p&gt;&lt;a name="cite_ref-33"&gt;&lt;/a&gt;&lt;a name="cite_ref-34"&gt;&lt;/a&gt;&lt;a name="cite_ref-35"&gt;&lt;/a&gt;&lt;a name="cite_ref-grida7_0-3"&gt;&lt;/a&gt;&lt;a name="cite_ref-36"&gt;&lt;/a&gt;&lt;a name="cite_ref-37"&gt;&lt;/a&gt;&lt;a name="cite_ref-38"&gt;&lt;/a&gt;&lt;a name="cite_ref-39"&gt;&lt;/a&gt;&lt;a name="cite_ref-40"&gt;&lt;/a&gt;&lt;a name="cite_ref-41"&gt;&lt;/a&gt; &lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;One predicted effect of an increase in solar activity would be a warming of most of the &lt;a href="http://en.wikipedia.org/wiki/Stratosphere"&gt;stratosphere&lt;/a&gt;, whereas an increase in greenhouse gases should produce cooling there.&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-33"&gt;[34]&lt;/a&gt; The observed trend since at least 1960 has been a cooling of the lower stratosphere.&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-34"&gt;[35]&lt;/a&gt; &lt;a href="http://en.wikipedia.org/wiki/Ozone_depletion"&gt;Reduction of stratospheric ozone&lt;/a&gt; also has a cooling influence, but substantial ozone depletion did not occur until the late 1970s.&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-35"&gt;[36]&lt;/a&gt; Solar variation combined with changes in &lt;a href="http://en.wikipedia.org/wiki/Volcano"&gt;volcanic activity&lt;/a&gt; probably did have a warming effect from pre-industrial times to 1950, but a cooling effect since.&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-grida7-0"&gt;[1]&lt;/a&gt; In 2006, Peter Foukal and colleagues found no net increase of solar brightness over the last 1,000 years. &lt;a href="http://en.wikipedia.org/wiki/Solar_cycle"&gt;Solar cycles&lt;/a&gt; led to a small increase of 0.07 percent in brightness over the last 30 years. This effect is too small to contribute significantly to global warming.&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-36"&gt;[37]&lt;/a&gt;&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-37"&gt;[38]&lt;/a&gt; One paper by Mike Lockwood and Claus Fröhlich found no relation between global warming and solar radiation since 1985, whether through variations in solar output or variations in &lt;a href="http://en.wikipedia.org/wiki/Cosmic_ray"&gt;cosmic rays&lt;/a&gt;.&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-38"&gt;[39]&lt;/a&gt; &lt;a href="http://en.wikipedia.org/wiki/Henrik_Svensmark"&gt;Henrik Svensmark&lt;/a&gt; and &lt;a href="http://en.wikipedia.org/wiki/Eigil_Friis-Christensen"&gt;Eigil Friis-Christensen&lt;/a&gt;, the main proponents of &lt;a href="http://en.wikipedia.org/wiki/Cloud_seeding"&gt;cloud seeding&lt;/a&gt; by galactic cosmic rays, disputed this criticism of their hypothesis.&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-39"&gt;[40]&lt;/a&gt; A 2007 paper found that in the last 20 years there has been no significant link between changes in cosmic rays coming to Earth and cloudiness and temperature.&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-40"&gt;[41]&lt;/a&gt;&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-41"&gt;[42]&lt;/a&gt;&lt;/span&gt;&lt;/p&gt; &lt;h3&gt;&lt;a name="Feedback"&gt;&lt;/a&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;Feedback&lt;/span&gt;&lt;/h3&gt; &lt;p&gt;&lt;i&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;Main article: &lt;a href="http://en.wikipedia.org/wiki/Effects_of_global_warming"&gt;Effects of global warming&lt;/a&gt;&lt;/span&gt;&lt;/i&gt;&lt;/p&gt; &lt;p&gt;&lt;a name="cite_ref-42"&gt;&lt;/a&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;When a warming trend results in effects that induce further warming, the process is referred to as a positive feedback; when the effects induce cooling, the process is referred to as a negative feedback. The primary positive feedback involves water vapor. The primary negative feedback is the effect of temperature on emission of infrared radiation: as the temperature of a body increases, the emitted radiation increases with the fourth power of its &lt;a href="http://en.wikipedia.org/wiki/Absolute_temperature"&gt;absolute temperature&lt;/a&gt;.&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-42"&gt;[43]&lt;/a&gt; This provides a powerful negative feedback which stabilizes the climate system over time.&lt;/span&gt;&lt;/p&gt; &lt;dl&gt;&lt;dt&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;&lt;a href="http://en.wikipedia.org/wiki/Water_vapor_feedback"&gt;Water 	vapor feedback&lt;/a&gt;  &lt;/span&gt; 	&lt;/dt&gt;&lt;dd style="margin-bottom: 0.2in;"&gt; 	&lt;a name="cite_ref-soden1_43-0"&gt;&lt;/a&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;One 	of the most pronounced positive feedback effects relates to the 	evaporation of water. If the atmosphere is warmed, the &lt;a href="http://en.wikipedia.org/wiki/Saturation_vapour_pressure"&gt;saturation 	vapour pressure&lt;/a&gt; increases, and the quantity of water vapor in 	the atmosphere will tend to increase. Since water vapor is a 	greenhouse gas, the increase in water vapor content makes the 	atmosphere warm further; this warming causes the atmosphere to hold 	still more water vapor (a &lt;a href="http://en.wikipedia.org/wiki/Positive_feedback"&gt;positive 	feedback&lt;/a&gt;), and so on until other processes stop the feedback 	loop. The result is a much larger greenhouse effect than that due to 	CO&lt;/span&gt;&lt;sub&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;2&lt;/span&gt;&lt;/sub&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt; 	alone. Although this feedback process causes an increase in the 	absolute moisture content of the air, the &lt;a href="http://en.wikipedia.org/wiki/Relative_humidity"&gt;relative 	humidity&lt;/a&gt; stays nearly constant or even decreases slightly 	because the air is warmer.&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-soden1-43"&gt;[44]&lt;/a&gt; 	&lt;/span&gt; 	&lt;/dd&gt;&lt;dt&gt; 	&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;Clouds  &lt;/span&gt; 	&lt;/dt&gt;&lt;dd style="margin-bottom: 0.2in;"&gt; 	&lt;a name="cite_ref-soden1_43-1"&gt;&lt;/a&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;Feedback 	effects due to clouds are an area of ongoing research. Seen from 	below, clouds emit infrared radiation back to the surface, and so 	exert a warming effect; seen from above, clouds reflect sunlight and 	emit infrared radiation to space, and so exert a cooling effect. 	Whether the net effect is warming or cooling depends on details such 	as the &lt;a href="http://en.wikipedia.org/wiki/List_of_cloud_types"&gt;type&lt;/a&gt; 	and altitude of the cloud, details that have been difficult to 	represent in climate models.&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-soden1-43"&gt;[44]&lt;/a&gt; 	&lt;/span&gt; 	&lt;/dd&gt;&lt;dt&gt; 	&lt;a href="http://en.wikipedia.org/wiki/Lapse_rate"&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;Lapse 	rate&lt;/span&gt;&lt;/a&gt;&lt;/dt&gt;&lt;dd style="margin-bottom: 0.2in;"&gt; 	&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;A subtler feedback process 	relates to changes in the &lt;a href="http://en.wikipedia.org/wiki/Lapse_rate"&gt;lapse 	rate&lt;/a&gt; as the atmosphere warms. The atmosphere's temperature 	decreases with height in the &lt;a href="http://en.wikipedia.org/wiki/Troposphere"&gt;troposphere&lt;/a&gt;. 	Since emission of infrared radiation varies with the fourth power of 	temperature, &lt;a href="http://en.wikipedia.org/wiki/Longwave_radiation"&gt;longwave 	radiation&lt;/a&gt; emitted from the upper atmosphere is less than that 	emitted from the lower atmosphere. Most of the radiation emitted 	from the upper atmosphere escapes to space, while most of the 	radiation emitted from the lower atmosphere is re-absorbed by the 	surface or the atmosphere. Thus, the strength of the greenhouse 	effect depends on the atmosphere's rate of temperature decrease with 	height: if the rate of temperature decrease is greater the 	greenhouse effect will be stronger, and if the rate of temperature 	decrease is smaller then the greenhouse effect will be weaker. Both 	theory and climate models indicate that with increased greenhouse 	gas content the rate of temperature decrease with height will be 	reduced, producing a negative &lt;/span&gt;&lt;i&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;lapse 	rate feedback&lt;/span&gt;&lt;/i&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt; that 	weakens the greenhouse effect. Measurements of the rate of 	temperature change with height are very sensitive to small errors in 	observations, making it difficult to establish whether the models 	agree with observations.&lt;/span&gt;&lt;/dd&gt;&lt;/dl&gt; &lt;p&gt; &lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;Aerial photograph showing a section of sea ice. The lighter blue areas are &lt;a href="http://en.wikipedia.org/wiki/Melt_ponds"&gt;melt ponds&lt;/a&gt; and the darkest areas are open water, both have a lower albedo than the white sea ice. The melting ice contributes to the &lt;a href="http://en.wikipedia.org/wiki/Ice-albedo_feedback"&gt;ice-albedo feedback&lt;/a&gt;.&lt;/span&gt;&lt;/p&gt; &lt;dl&gt;&lt;dt&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;&lt;a href="http://en.wikipedia.org/wiki/Albedo"&gt;Ice-albedo&lt;/a&gt;  	&lt;/span&gt; 	&lt;/dt&gt;&lt;dd style="margin-bottom: 0.2in;"&gt; 	&lt;a name="cite_ref-45"&gt;&lt;/a&gt;&lt;a name="cite_ref-46"&gt;&lt;/a&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;Another 	important feedback process is &lt;a href="http://en.wikipedia.org/wiki/Ice-albedo_feedback"&gt;ice-albedo 	feedback&lt;/a&gt;.&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-45"&gt;[46]&lt;/a&gt; 	When global temperatures increase, ice near the poles melts at an 	increasing rate. As the ice melts, land or open water takes its 	place. Both land and open water are on average less reflective than 	ice, and thus absorb more solar radiation. This causes more warming, 	which in turn causes more melting, and this cycle continues. Rapid 	&lt;a href="http://en.wikipedia.org/wiki/Arctic_shrinkage"&gt;Arctic 	shrinkage&lt;/a&gt; is already occurring, with 2007 being the lowest ever 	recorded &lt;a href="http://en.wikipedia.org/wiki/Sea_ice"&gt;sea ice&lt;/a&gt; 	area. Some models suggest that &lt;a href="http://en.wikipedia.org/wiki/Tipping_point_%28climatology%29"&gt;tipping 	points&lt;/a&gt; exist, leading to a potentially rapid collapse of &lt;a href="http://en.wikipedia.org/wiki/Sea_ice"&gt;sea 	ice&lt;/a&gt; cover in the &lt;a href="http://en.wikipedia.org/wiki/Arctic"&gt;Arctic&lt;/a&gt;.&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-46"&gt;[47]&lt;/a&gt; 	&lt;/span&gt; 	&lt;/dd&gt;&lt;dt&gt; 	&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;&lt;a href="http://en.wikipedia.org/wiki/Arctic_methane_release"&gt;Arctic 	methane release&lt;/a&gt;  &lt;/span&gt; 	&lt;/dt&gt;&lt;dd style="margin-bottom: 0.2in;"&gt; 	&lt;a name="cite_ref-47"&gt;&lt;/a&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;Warming 	is also the triggering variable for the release of methane from 	sources both on land and on the deep ocean floor, making both of 	these possible feedback effects. Thawing &lt;a href="http://en.wikipedia.org/wiki/Permafrost"&gt;permafrost&lt;/a&gt;, 	such as the frozen &lt;a href="http://en.wikipedia.org/wiki/Peat"&gt;peat&lt;/a&gt; 	&lt;a href="http://en.wikipedia.org/wiki/Bog"&gt;bogs&lt;/a&gt; in &lt;a href="http://en.wikipedia.org/wiki/Siberia"&gt;Siberia&lt;/a&gt;, 	creates a &lt;a href="http://en.wikipedia.org/wiki/Positive_feedback"&gt;positive 	feedback&lt;/a&gt; due to the potentially rapid release of CO&lt;/span&gt;&lt;sub&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;2&lt;/span&gt;&lt;/sub&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt; 	and CH&lt;/span&gt;&lt;sub&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;4&lt;/span&gt;&lt;/sub&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;.&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-47"&gt;[48]&lt;/a&gt;[&lt;/span&gt;&lt;a href="http://en.wikipedia.org/wiki/Wikipedia:Reliable_sources"&gt;&lt;i&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;unreliable 	source?&lt;/span&gt;&lt;/i&gt;&lt;/a&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;] 	Methane discharge from permafrost is presently under intensive 	study.[&lt;/span&gt;&lt;a href="http://en.wikipedia.org/wiki/Wikipedia:Citation_needed"&gt;&lt;i&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;citation 	needed&lt;/span&gt;&lt;/i&gt;&lt;/a&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;] &lt;/span&gt; 	&lt;/dd&gt;&lt;dt&gt; 	&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;&lt;a href="http://en.wikipedia.org/wiki/Clathrate_gun_hypothesis"&gt;Clathrate 	gun hypothesis&lt;/a&gt;  &lt;/span&gt; 	&lt;/dt&gt;&lt;dd style="margin-bottom: 0.2in;"&gt; 	&lt;a name="cite_ref-48"&gt;&lt;/a&gt;&lt;a name="cite_ref-49"&gt;&lt;/a&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;Warmer 	deep ocean temperatures could also release the greenhouse gas 	&lt;a href="http://en.wikipedia.org/wiki/Methane"&gt;methane&lt;/a&gt; from the 	'frozen' state of the vast deep ocean deposits of &lt;a href="http://en.wikipedia.org/wiki/Methane_clathrate"&gt;methane 	clathrate&lt;/a&gt;, according to the &lt;a href="http://en.wikipedia.org/wiki/Clathrate_Gun_Hypothesis"&gt;Clathrate 	Gun Hypothesis&lt;/a&gt;, albeit over millenial time-scales. A further 	release of methane from shallow cold water clathrates is also 	expected, and is predicted to be faster.&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-48"&gt;[49]&lt;/a&gt; 	Buffett and Archer predict a large release of &lt;a href="http://en.wikipedia.org/wiki/Methane"&gt;methane&lt;/a&gt; 	in response to warming, and a large increase in methane stores if 	oxygen levels in the ocean fall.&lt;a href="http://en.wikipedia.org/wiki/Global_warming#cite_note-49"&gt;[50]&lt;/a&gt; 	They offer a "global estimate of 3×10&lt;/span&gt;&lt;sup&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;18&lt;/span&gt;&lt;/sup&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt; 	g of carbon (3000 Gton C) in clathrate and 2×10&lt;/span&gt;&lt;sup&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;18&lt;/span&gt;&lt;/sup&gt;&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt; 	g (2000 Gton C) in methane bubbles. The predicted methane inventory 	decreases by 85% in response to 3 °C of warming. Conversely, the 	methane inventory increases by a factor of 2 if the O2 concentration 	of the deep ocean decreases by 40 μM or carbon rain increases by 	50%" &lt;/span&gt; 	&lt;/dd&gt;&lt;dt&gt; 	&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;Sequestration  &lt;/span&gt; 	&lt;/dt&gt;&lt;dd style="margin-bottom: 0.2in;"&gt; 	&lt;span style="background: transparent none repeat scroll 0% 0%; -moz-background-clip: -moz-initial; -moz-background-origin: -moz-initial; -moz-background-inline-policy: -moz-initial;"&gt;Ocean ecosystems' ability to 	sequester carbon are expected to decline as it warms. This is 	because the resulting low nutrient levels of the &lt;a href="http://en.wikipedia.org/wiki/Mesopelagic_zone"&gt;mesopelagic 	zone&lt;/a&gt; (about 200 to 1000 m depth) limits the growth of &lt;a href="http://en.wikipedia.org/wiki/Diatom"&gt;diatoms&lt;/a&gt; 	in favor of smaller &lt;a href="http://en.wikipedia.org/wiki/Phytoplankton"&gt;phytoplankton&lt;/a&gt; 	that are poorer &lt;a href="http://en.wikipedia.org/wiki/Biological_pump"&gt;biological 	pumps&lt;/a&gt; of carbon.&lt;/span&gt;&lt;/dd&gt;&lt;/dl&gt; &lt;p style="margin-bottom: 0in;"&gt;&lt;br /&gt;&lt;/p&gt; </description><thr:total xmlns:thr="http://purl.org/syndication/thread/1.0">0</thr:total></item><item><title>Crackdown on political activists continues</title><link>http://top-tips-today.blogspot.com/2009/03/crackdown-on-political-activists.html</link><category>top</category><author>noreply@blogger.com (puwokertoinfo)</author><pubDate>Sun, 8 Mar 2009 20:04:00 -0700</pubDate><guid isPermaLink="false">tag:blogger.com,1999:blog-4583422652989818656.post-4816381290330047088</guid><description>&lt;h2 align="center"&gt;&lt;span style="color:#003366;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/h2&gt;&lt;h5 align="center"&gt; &lt;/h5&gt;&lt;br /&gt;&lt;p style="text-indent: 15px; margin-left: 3px; margin-right: 3px; margin-top: 1px;" align="justify"&gt;&lt;span style="font-size:100%;"&gt;ISLAMABAD, Mar 13: Authorities in Pakistan''s north-west have banned political gatherings and a protest convoy has been halted in Sindh as a crackdown on activists spreads, reports BBC.&lt;br /&gt;Dozens of lawyers and political leaders were arrested in North West Frontier Province (NWFP) overnight, reports BBC.&lt;br /&gt;Protesters have been trying to reach Islamabad by Monday on a "long march" that is demanding the reinstatement of sacked judges.&lt;br /&gt;The government says the march is aimed at destabilising the country.&lt;br /&gt;The protest is causing widening international concern.&lt;br /&gt;US special envoy to Pakistan and Afghanistan, Richard Holbrooke, and British Foreign Secretary David Miliband both spoke to President Asif Ali Zardari on Thursday.&lt;br /&gt;Protest organisers had intended the four-day march from cities across Pakistan to culminate in a sit-in at the parliament in Islamabad, on Monday.&lt;br /&gt;However, the BBC''s Syed Shoaib Hasan in Islamabad says that while protests will continue throughout Pakistani cities and activists may try to reach the capital in small groups, the crackdown has effectively ended the "long march".&lt;br /&gt;Protest organisers say that more than 1,000 opposition leaders and activists have already been jailed or put under house arrest.&lt;br /&gt;Police in NWFP overnight arrested dozens of lawyers, political leaders, legislators and activists in the districts of Peshawar, Mardan, Abbottabad and Mansehra.&lt;br /&gt;Raids are still going on in the area amid reports that many opposition leaders and lawyers have gone into hiding to avoid arrest.&lt;br /&gt;Gatherings have been banned and large contingents of police have been deployed to prevent activists from proceeding to Islamabad in large groups.&lt;br /&gt;Police also blocked a convoy of protesters led by the president of the Supreme Court bar association, Ali Ahmed Kurd, as it tried to enter Sindh province on its way to the capital.&lt;br /&gt;Punjab and Sindh provinces have both banned political gatherings.&lt;br /&gt;Kurd said he "strongly condemned the Sindh government for stopping our peaceful march".&lt;br /&gt;" I don''t think [President Zardari] will be able to complete his five years "&lt;br /&gt;Nawaz Sharif&lt;br /&gt;He added: "We will try to reach Islamabad by other routes and appeal to all Pakistanis to reach Islamabad in groups or as individuals by any possible means.&lt;br /&gt;"This action of the government has shown to the people of Pakistan and the entire world that lawyers cannot move freely in their own country."&lt;br /&gt;On Thursday, the police in Karachi, the capital of Sindh province, baton charged to disperse protesting lawyers and political activists.&lt;br /&gt;Lawyers in Karachi say they will boycott all courts on Friday.&lt;br /&gt;The government fears the protest could turn more violent.&lt;br /&gt;The US has expressed its concern about the situation.&lt;br /&gt;In addition to the Holbrooke call, US ambassador to Pakistan Anne Patterson met Prime Minister Yusuf Raza Gilani.&lt;br /&gt;US state department spokesman Robert Wood said the US was stressing that violence should be avoided, the rule of law respected and that peaceful protests should be allowed to proceed.&lt;br /&gt;The protest follows a heightening of tensions in Pakistan, after a court ruling barring opposition PML-N party leader Nawaz Sharif and his brother from holding public office.&lt;br /&gt;Sharif has backed the lawyers'' demand for the judges to be reinstated and has called on Pakistanis to join the demonstration.&lt;br /&gt;He said that Mr Zardari''s refusal to meet the demand was "shortening his political life".&lt;br /&gt;"I don''t think he will be able to complete his five years," Mr Sharif said.&lt;br /&gt;The sackings in November 2007 of some 60 senior judges, including the then-chief justice Iftikhar Chaudhry, sparked countrywide protests and ultimately led to President Pervez Musharraf''s resignation.&lt;br /&gt;Zardari''s critics argue that he fears the chief justice could revive corruption cases against him.&lt;br /&gt;Six months after Zardari took office, Pakistan is descending deeper into crisis, correspondents say.&lt;br /&gt;The BBC''s Barbara Plett in Islamabad says many believe that Mr Sharif''s backing of the protesters has turned the march into a power struggle that the country can ill afford. &lt;/span&gt;&lt;/p&gt;</description><thr:total xmlns:thr="http://purl.org/syndication/thread/1.0">0</thr:total></item></channel></rss>