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Observations of anthropogenic global warming

Archive for March, 2013

New research from early 2013

Posted by Ari Jokimäki on March 19, 2013

Since the end of the New research from last week series I have been noting new research papers in Twitter and in Facebook. For those who don’t follow those places, below are my new paper tweets since the beginning of 2013 to this day. There are 211 of them, which surprised me a little, because it’s almost 3 papers per day. I thought I would have averaged below 2 per day. So, here they are all mixed up (subject-wise, they actually are in temporal order so that latest is first):

1. Climate change is unlikely to dramatically reduce overall winter mortality rates

2. Future grand solar minimum could slow down but not stop global warming

3. More hurricanes to hit Western Europe due to global warming

4. The stability of an evolving Atlantic meridional overturning circulation

5. Recent intense hurricane response to global climate change (open access)

6. Decades of observations are needed to determine cloud feedbacks

7. Over 21000 years old dissolved organic permafrost carbon was found in stream from Siberia

8. Atlantic Multidecadal Oscillation’s structure and climate footprint

9. Nonlinear effects of elevated temperature on grapevine phenology

10. Has Northern Hemisphere been warming during the boreal winter of last few decades?

11. Climate Impacts of a Large-Scale Biofuels Expansion

12. Climate impact of stratospheric ozone recovery

13. Potential for rooftop photovoltaics in Tokyo to replace nuclear capacity (open access)

14. Implications of a break-up of China for carbon dioxide emissions

15. Parameterization of Wind Farms in Climate Models

16. The economic impact of climate change in the 20th and 21st centuries

17. Tropical coral reef habitat in a geoengineered, high-CO2 world

18. Extended season for northern butterflies

19. Cold winter extremes in northern continents linked to Arctic sea ice loss (open access)

20. Recalculating GHG emissions saving of palm oil biodiesel (open access)

21. Cosmic ray modulation of infra-red radiation in the atmosphere (only a small effect on climate)

22. Achieving Climate Change Absolute Accuracy in Orbit

23. Impacts of climate change on avian populations

24. On the origin of multidecadal to centennial Greenland temperature anomalies over the past 800 yr (open access)

25. CMIP5 simulations might underestimate risk of prolonged droughts under climate change in western North America

26. Vertical structure of warming consistent with upward shift in middle and upper troposphere

27. Anthropogenic climate change may directly influence ENSO

28. Important role for CO2 at past climate change transitions

29. Vulnerability of calcifying larval stage of Antarctic sea urchin to ocean acidification and warming

30. High tolerance of microzooplankton to ocean acidification in an Arctic coastal plankton community (open access)

31. Life histories predict coral community disassembly under multiple stressors

32. Shutdown and recovery of the AMOC in a coupled global climate model

33. A new mechanism for Dansgaard-Oeschger cycles

34. CO2 plays a large role in observed temperature trend at Antarctic Peninsula’s Faraday/Vernadsky station

35. When will the summer arctic be nearly sea ice free?

36. Winter weather versus group thermoregulation: what determines survival in hibernating mammals?

37. Kilimanjaro likely to be ice-free before 2060 if current climatological conditions are maintained (open access)

38. Anthropogenic carbon dioxide source areas observed from space (open access)

39. Climate change reduces the net sink of CH4 and N2O in a semiarid grassland

40. Vulnerability of Terrestrial Island Vertebrates to Projected Sea-Level Rise

41. Southeastern U.S. anomalous cooling in the 20th century

42. Anthropogenic effects on the subtropical jet in the Southern Hemisphere (open access)

43. Effect of cloudiness on long-term variability in air temperature in Krakow

44. Improved ice bed, surface and thickness datasets for Antarctica (open access)

45. Climate Change Impacts on Global Agricultural Water Deficit

46. Observed trends in the global jet stream characteristics during the second half of the 20th century

47. There truly are mushroom clouds (open access)

48. Analysis of global methane changes after the 1991 Pinatubo volcanic eruption (open access)

49. Icelandic ice caps contribute to sea level rise too

50. Human-induced changes to atmospheric composition affects global mean surface temperature changes

51. Detection and attribution of anthropogenic climate change impacts

52. Australian Great Flood of 1954: Estimating the cost of a similar event in 2011

53. Impacts of global warming on Northern Hemisphere winter storm tracks

54. Sea ice loss is weakening the oceanic CO2 sink in Canada Basin

55. Anthropogenic influence is clearly detectable in extreme temperatures over China

56. Evolution of the subglacial drainage system beneath the Greenland Ice Sheet revealed by tracers

57. Mass loss of Greenland’s glaciers and ice caps 2003-2008

58. Vegetation-related roughness is possible cause of recent decrease in dust emission from Sahel

59. Global wind power resource estimates might be substantially overstated (open access)

60. Invitation for researchers to study information stored in cave ice deposits before they melt away

61. No cumulative effect of 10 years of elevated CO2 on perennial plant biomass components in Mojave Desert

62. Diagnosing Present and Future Permafrost from Climate Models

63. Irreversible mass loss of Canadian Arctic Archipelago glaciers

64. Potential for evolutionary responses to climate change – evidence from tree populations

65. Projected Changes in East African Rainy Seasons

66. NDVI data for 1982–2006 indicates CO2 fertilization effect in global vegetation

67. Surface elevation and velocity changes on the south-central Greenland ice sheet: 1980-2011

68. Accelerating shrinkage of Patagonian glaciers from the Little Ice Age

69. From this abstract I can’t tell if there will be more suitable or unsuitable panda habitat but I’m guessing latter

70. Warm-season severe wind events in Germany

71. Extreme hail day climatology in Southwestern France

72. New generation of climate models agree better with observations

73. Space–time distribution of tornado events in Bulgaria (1956–2010)

74. Impacts of ocean acidification on marine organisms

75. Snow variability in Romania in connection to large-scale atmospheric circulation

76. Severe thunderstorms and climate change

77. Permafrost soils – initial carbon sink but eventually possible carbon source (open access)

78. The upper end of climate model temperature projections is inconsistent with past warming (open access)

79. Synchronous fluctuations of glaciers in the Alps and Altai in the second half of the Holocene

80. The contribution of radiative feedbacks to orbitally-driven climate change

81. Likely Ranges of Climate Change in Bolivia

82. Strong increase in convective precipitation in response to higher temperatures

83. Predator-induced reduction of freshwater carbon dioxide emissions

84. Rapid climatic driven shifts of diatoms at high latitudes

85. Modelled Rapid Adjustments in Diurnal Temperature Range Response to CO2 and Solar Forcings

86. The strength of the holiday effect is mainly caused by the degree of urbanization

87. In addition to warming and acidification, mankind also does other bad things to coral reefs

88. Global precipitation trends: larger than expected increase over oceans, over land trends are what IPCC AR4 says

89. Storm intensity has increased in San Francisco Bay Area between 1890 and 2010

90. Anthropogenic Impact on Agulhas Leakage

91. Global nutrient limitation in terrestrial vegetation

92. Climate warming shifts carbon allocation from stemwood to roots in calcium-depleted spruce forests

93. Vietnam has warmed about twice the rate of global warming since 1970’s

94. Why was there an increase in carbon-14 production in AD 774-775?

95. A new global reconstruction of temperature changes at the Last Glacial Maximum (open access)

96. A review of sea ice proxy information from polar ice cores

97. Optimal fingerprinting finds the effect of anthropogenic forcings including land use in daily extreme temperatures

98. Anthropogenic influences have made substantial contribution to evolution of free atmosphere temperatures

99. Yet another attribution study shows anthropogenic GHG’s dominating global warming since mid 20th century

100. Human-induced climate change was one of the causes of 2011 East African drought

101. Arctic sea ice cover may have passed a tipping point in 2007 (open access)

102. Loss of plant biodiversity eliminates stimulatory effect of elevated CO2 on earthworm activity in grasslands

103. Artificial light pollution: are shifting spectral signatures changing the balance of species interactions?

104. Detrimental effects of Ocean Acidification on the economically important Mediterranean red coral

105. Distribution of ant species shifts to higher elevations with minimum temperature increase

106. CO2 stimulation has not been enough to counteract warming induced drought stress in Mexican high altitude forests

107. Modes and Mechanisms of Global Water Vapor Variability over the 20th Century

108. The transient versus the equilibrium response of sea ice to global warming

109. Antarctic ozone loss in 1979–2010: first sign of ozone recovery (open access)

110. Accelerated glacier melt in 2002 – 2007 over the Bering Glacier in Alaska

111. Ice cores from Antarctica and Greenland improve our knowledge of volcanic forcing over last 2000 years

112. Spatial distribution of temperature trends in Sicily

113. New shaving technique to release trapped air for measurements from ice core samples

114. Important role of mid-tropospheric atmospheric circulation in recent surface melt increase over Greenland

115. Controls of Global Snow Under a Changed Climate

116. How much land based GHG can be achieved without compromising food security and environmental goals?

117. Dansgaard–Oeschger events: bifurcation points in the climate system (open access)

118. Ocean acidification and warming scenarios increase microbioerosion of coral skeletons

119. The Medieval Climate Anomaly and the Little Ice Age in the eastern Ecuadorian Andes (open access)

120. Ice sheet sources of sea level rise and freshwater discharge during the last deglaciation

121. Surface albedo feedbacks from climate variability and change

122. Stratospheric ozone depletion has contributed to Hadley cell expansion

123. Snow variability in the Swiss Alps 1864–2009

124. Using phenology to assess urban heat islands in tropical and temperate regions

125. Quaternary history of sea ice in the western Arctic Ocean based on foraminifera

126. What would super eruption of the Yellowstone volcanic system do to global climate and carbon cycle (open access)

127. Arctic microbial community dynamics influenced by elevated CO2 levels (open access)

128. Interhemispheric temperature asymmetry over the 20th century and in future projections

129. Relationship between Winter Sea Ice and Summer Atmospheric Circulation over Eurasia

130. How wind farms affect local weather

131. Past history and future fate of Arctic small mammals in a changing climate

132. Greenland meltwater lakes have expanded substantially inland to higher elevations with warming

133. Ocean acidification effects on Arctic microbial community dynamics (open access)

134. Environmental controls on the thermal structure of alpine glaciers (open access)

135. A 2°C warmer world is not safe for ecosystem services in the European Alps

136. A synthesis and review of Holocene paleofire records and their controls

137. Predictability of twentieth century sea-level rise from past data

138. Anthropogenic changes in the dynamics of the mesosphere

139. Global shifts towards positive species interactions with increasing environmental stress

140. Reconstruction of northeast Asia spring temperature 1784–1990 (open access)

141. Can black carbon in snow be detected by remote sensing? Not likely, says a new study

142. Increased summer rainfall in northwest Australia linked to southern Indian Ocean climate variability

143. Quantifying the effect of urbanization on U.S. Historical Climatology Network temperature records

144. Quantification of methane emission rates from coal mine ventilation shafts

145. An estimate of global glacier volume

146. Global river discharge and water temperature under climate change

147. Detectable Changes in the Frequency of Temperature Extremes

148. An assessment of the Atlantic and Arctic sea–air CO2 fluxes, 1990–2009 (open access)

149. How will climate change modify river flow regimes in Europe?

150. CryoSat-2 estimates of Arctic sea ice thickness and volume

151. Climate change is expected to decrease C4 crop yields in Africa and India by 2100

152. The impact of an intense summer cyclone on 2012 Arctic sea ice retreat

153. Arctic climate warming and sea ice declines lead to increased storm surge activity

154. CO2 forcing decreases maximum strength of the Atlantic meridional overturning circulation

155. Simultaneous shifts in temperature in Central Europe and Greenland during the last deglaciation

156. Global hot-spots of heat stress on agricultural crops due to climate change

157. Estimating impacts of warming temperatures on California’s electricity system

158. Staying cool in a changing climate

159. Where do winds come from? (open access)

160. The carbon budget of South Asia (open access)

161. Does Antarctic glaciation cool the world? (open access)

162. Short-term weather and belief in anthropogenic climate change

163. Updated analyses of temperature and precipitation extreme indices since the beginning of 20th century

164. Current state of glaciers in the tropical Andes (open access)

165. Decadal record of satellite carbon monoxide observations (open access)

166. Dessler’s 2010 results of positive short-term cloud feedback seem to be robust

167. A 600,000 year Arctic sea-ice record from Mendeleev Ridge based on ostracodes

168. Revised estimates of Greenland ice sheet thinning histories based on ice-core records

169. Change in snow phenology and its potential feedback to temperature in the Northern Hemisphere (open access)

170. The Suess effect in Fiji coral carbon-13 and its potential as a tracer of anthropogenic CO2 uptake

171. Evidence of current impact of climate change on life

172. Trends in ISCCP, MISR and MODIS Cloud-Top-Height and Optical-Depth Histograms

173. Changepoint Detection in Climatic Time Series with Long-term Trends

174. Elevated emissions from high-latitude wetlands contributed to early Holocene high CH4 concentration

175. High predictive skill of global surface temperature a year ahead

176. Improving the temporal and spatial distribution of CO2 emissions from global fossil fuel emission data sets

177. The Roles of Aerosol Direct and Indirect Effects in Past and Future Climate Change

178. Land water contribution to sea level from GRACE and Jason measurements

179. Influence of climate variability on seasonal extremes over Australia

180. Arctic climate sensitivity to local black carbon

181. Increased variability in cold-season temperature since the 1930s in subtropical China

182. Assessment of global cloud datasets from satellites

183. Cloud and water vapor feedbacks are still biased in CMIP5 models

184. No divergence in a 1200 year tree-ring temperature reconstruction at the northern European treeline

185. Clouds become fewer, higher, and thicker, and net cloud feedback is positive in most CMIP5 models

186. An analysis of the short-term cloud feedback using MODIS data

187. On the use of elevation, altitude, and height in the ecological and climatological literature

188. Global all-sky shortwave direct radiative forcing of anthropogenic aerosols

189. Global analysis of night marine air temperature and its uncertainty since 1880

190. Sea surface temperature was lower than today during Medieval Warm Period in Southern Adriatic Sea region

191. Global warming in an independent record of the past 130 years

192. High emission of carbon dioxide and methane during ice-thaw in high latitude lakes

193. There is high probability for black carbon emissions to have positive forcing and warm the climate

194. Climatic impact of Changbaishan volcano eruption in 10th century might have been only regional

195. 20th Century summer sunshine levels possibly similar to the Mediæval period in Swedish reconstruction

196. Summer 1540 might have been warmer in Switzerland than summer 2003 (open access)

197. Site factors and tree age can be more important drivers of growth trends in arctic treelines than climate

198. In contrast to northern Europe the YD event had no major effect on mammals in Switzerland

199. Soil warming increases alpine plant species richness but decreases germination from soil seed bank

200. Fragmentation and climate warming interact to affect persistence of native trout in the Colorado River basin

201. Fossil plants used for CO2 reconstruction from Late Oligocene to Early Miocene

202. Global anthropogenic sulfur dioxide emissions 2000-2011 (open access)

203. Roe deer in forest habitats cannot currently cope with increasingly early springs

204. In Arctic, local black carbon causes cooling while remote black carbon causes warming (open access)

205. Enhanced flooding due climate change can result in rapid emissions of stored carbon in soils

206. Expected decrease of tropical cyclones in Southern Gulf of Mexico/Caribbean and increase over central Atlantic

207. Observations and models agree on temperature trends in Southern Hemisphere stratosphere

208. Analysis of temperature extremes in Australia from 1910 to 2010

209. Are climate model simulations of clouds improving?

210. Early Holocene summer temperatures may have been 2.3°C above modern ones in Swedish Scandes

211. Changes in soil biotic activity might make Arctic substantial carbon source and Antarctica a carbon sink

Posted in Climate science | 5 Comments »

What doesn’t change with climate?

Posted by Ari Jokimäki on March 8, 2013

Global warming and subsequent climate change have a lot of different effects. The composition of the atmosphere changes. The troposphere swells and the atmosphere gets wetter. Oceans warm and expand. There are chemical changes in the ocean waters. Well known example of that is the ocean acidification caused by the increasing carbon dioxide concentration.

The biosphere gets shuffled. Some species shift to other places looking for more suitable conditions in which to live. Body shape and/or size changes for some species. The timetables between species get all mixed up. For example, because of an earlier spring the available food (caterpillars) is gone before the eggs of migratory birds hatch. Some, or according to predictions quite many, of the species will even go extinct.

Glaciers and ice sheets are melting. There are changes even in the lithosphere when the pressing weight of the ice sheets and glaciers is reduced as they melt into the ocean. Today at some places we can still see this same effect at work as the Earth’s crust is uplifting because the weight of the ice sheets that were there during the last glaciation (i.e. the “ice age”) was removed when the ice melted away. This effect also affects the asthenosphere, a viscous layer below the lithosphere.

So the climate change shows up everywhere – in the atmosphere, hydrosphere, biosphere, cryosphere, lithosphere, asthenosphere, and beyond. Is there anything within Earth’s system that doesn’t change with climate?

Read the rest of this entry »

Posted in Uncategorized | 2 Comments »

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