Annual surface temperatures (GISS) for the year 2009 compared to average 1998-2006:  72N-60S   Arctic   Antarctic 2 2 22
 Monthly surface temperatures (GISS) for June 2010 compared to average 1998-2006:  72N-60S   Arctic   Antarctic 2 2
 Latest global monthly temperature estimate:  UAH   RSS   HadCRUT3   NCDC   GISS  2
 Change over time of global monthly temperature estimates:   UAH   RSS   HadCRUT3   NCDC   GISS   C2
 CO2 and global monthly surface temperature estimates:   CO2   HadCRUT3   NCDC   GISS
 Sea surface temperature estimates:   UAH   HadSST2   NCDC   2
 Sea level:    SeaLevelChange   SeaLevelChangeRate   2
 Sea ice: Arctic and Antarctic:   NSIDCnow   IRAC-JAXAnow   NSIDCsince1978   2
 Snow cover:   Northern hemisphere   Europe-Asia   Alaska-Canada  USA-Canada 2 
 For those who want a more comprehensive, but still rapid monthly or annual climatic update: 2 March2009   April 2009   May2009  June 2009  July 2009  August2009   September2009   October2009   November2009   December2009   YEAR2009   January2010   February2010   March2010   April2010   May2010   June2010

 

Click here for information about book on climate published 30 November 2009. Now also as e-book.

 

About this web site: Climate4you

The objective of the present web site is to provide information on meteorological and climatologically issues of general and specific interest. The purpose is not to provide a forum for discussions. Many fine web sites take care of this. Some recent debates, books and other initiatives relating to global climatic changes, however, apparently are frustrated by a certain lack of knowledge on updated meteorological conditions and their variations in time and space. Also when it comes to the likely effects of climate change, the lessons of history often appear to be unknown or forgotten. In Europe it is only little more than 200 years since the recognition that Earth is a dynamic planet began to transpire as a result of basic geological research. Previously, in Europe it was widely believed that Earth essentially was unchanging, and only about 6000 years old according to a study of the Bible by James Ussher (1581-1656), the Anglican Archbishop of Armagh, Ireland. Today it is equally easy to forget that it is only about 160 years since about one million people in Europe died of starvation and epidemic diseases because of climate-induced harvest failures

The main emphasis of the present web site is therefore to provide the interested reader with data and other information on meteorology and climate. Climate change information needs to be both accurate and undistorted, and analysis unemotional. Respecting the notion that information always should be the starting point for personal thought, analysis and interpretation, links to sources (digital and written) are provided throughout the web site. It is definitely not the purpose to encourage a passive personal approach by providing a list of 'correct' answers to a list of 'key' questions, but rather to stimulate active, personal thought and analysis. 

The least objective part of the present web site is presumably the section on 'Climate Reflections', which is constructed around some of the webmaster's personal interpretations of certain data series. A slightly longer essay (in Norwegian) on the general climate theme can be downloaded by clicking here.

The recent focus on climate change has resulted in an increased awareness that climate is not as constant as it may have appeared previously. In this context, even the most extreme and divergent forecasts of future climate may have done some good. This is, however, a situation that should not continue much longer, as it confuses and disillusionates political decision-makers and the general public about the value of so-called ‘climate experts’. In addition, the initial humble scientific attempts of modelling the future climate have unfortunately developed into a large-scale example of groupthink with its own dynamics, making informed political judgment difficult.

Air temperature remains a central theme in discussions on global climate change, and admirable attempts to estimate the global temperature have been published by different research teams or -institutions. However, a number of issues relating to obtaining representative measurements of surface air temperature still remains, especially in or near areas affected by urban development. Even in Arctic regions it might be difficult to obtain representative air temperature measurements, despite all professional efforts. Also the varying degree of temporal stability displayed by the various global temperature records deserves attention. 

The difficulty of identifying a new climatic trend deviating from a background of natural variations is therefore real and constitutes an important difficulty for both scientists and policy-makers. As an example: Is it possible to conclude that the late 20th century global temperature increase is unique in relation to previous temperature increases? Or, alternatively, could it just as well represent part of the natural temperature increase following the end of the Little Ice Age ? Click here to read a few reflections on this interesting question. Another important issue is the changing relationship between atmospheric CO2 and global temperature in recent times ?

The immediate need for climate scientists appears to be improving empirical knowledge on climate change, past and present, and to understand the limitations of the different types of approach to forecasting climate. For the decision-makers the lesson presumably is to allow wider margins for future climatic change; cooler as well as warmer, wetter as well as drier, windier as well as less windy, etc. Preparing for warming only may not be entirely prudent. Climate science remains a highly complex issue where simplification tends to lead to confusion, and where understanding requires knowledge, openness to new hypotheses, thought and effort.

The present website is still under development, and updates and new material will be added from time to time. A list of the latest key updates are shown in the lower part of the panel to the left. Thank you for your interest.

 

Yours sincerely, Ole Humlum

Click here for bibliography.

 

Latest update July 29, 2010.

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