PENGGUNAAN MODEL PEMBELAJARAN INKUIRI TERBIMBING UNTUK MENINGKATKAN HASIL BELAJAR PESERTA DIDIK

Penelitian ini dilatar belakangi oleh rendahnya sikap rasa ingin tahu dan hasil belajar peserta didik pada Subtema Makananku Sehat dan Bergizi yang pencapaiannya hanya 35% peserta didik yang tuntas memenuhi nilai KKM. Selain itu pendidik masih menggunakan metode atau model pembelajaran yang bersifat teacher centered, yaitu model ceramah.Pelaksanaan yang dilakukan peneiti yaitu dua siklus dan setiap siklus terdiri dari 3 pembelajaran.Model Pembelajaran yang digunakan peneliti yaitu inkuiri terbimbing, pengertian dari inkuiri terbimbing merupakan model pembelajaran yang memberikan kesempatan kepada peserta didik untuk aktif terlibat dalam proses pembelajaran dengan melakukan penyelidikan dan pemecahan masalah secara mandiri namum tetap dengan bimbingan pendidik agar peserta didik lebih mudah dalam memahami konsep pelajaran. Subjek penelitian ini adalah siswakelas IV D SDN Leuwipanjang dengan jumlah peserta didik sebanyak 35 orang. Instrument pembelajaran yang digunakan adalah berupa tes, lembar observasi (observasi pendidik dan observasi peserta didik), LKPD (Lembar Kerja Peserta Didik) dan lembar angket. Hasil penelitian dengan menggunakan model pembelajaran inkuiri terbimbing ditunjukan dengan perencanaan setiap siklusnya yang mengalami perbaikan berdasarkan hasil refleksi di siklus sebelumnya. Pelaksanaan pembelajaran dengan menggunakan model pembelajaran inkuiri terbimbing dapat dilihat dari aktivitas pendidik dan peserta didik pada setiap siklusnya yang mengalami peningkatan. Pencapaian hasil belajar afektif mencapai 44% pada siklus II mencapai 80% dan kognitif peserta didik pada siklus I mencapai rata-rata 35% Siklus II ketuntasan 80%. Adapun hasil belajar psikomotor peserta didik di siklus I mencapai ketuntasan 36%. Siklus II mencapai mencapai ketuntasan 88%. Ambatan yang dilami oleh peneiti yaitu alokasi waktu dan pengelolaan kelas, Upaya yang dilakukan peneliti adalah mengatur pelaksannaan pembelajaran sesuai dengan rencana yang kita persiapkan dengan baik dan mengatur suasana kelas dengan menyenangkan yaitu membuat media pembelajaran yang baik sehingga daapat menarik minat belajar peserta didik. Kata Kunci : Inkuiri Terbimbing, rasa ingin tahu, hasil belajar peserta didik, hambatan pelaksanaan, upaya peningkata

Intercomparison of the northern hemisphere winter mid-latitude atmospheric variability of the IPCC models

We compare, for the overlapping time frame 1962-2000, the estimate of the northern hemisphere (NH) mid-latitude winter atmospheric variability within the XX century simulations of 17 global climate models (GCMs) included in the IPCC-4AR with the NCEP and ECMWF reanalyses. We compute the Hayashi spectra of the 500hPa geopotential height fields and introduce an integral measure of the variability observed in the NH on different spectral sub-domains. Only two high-resolution GCMs have a good agreement with reanalyses. Large biases, in most cases larger than 20%, are found between the wave climatologies of most GCMs and the reanalyses, with a relative span of around 50%. The travelling baroclinic waves are usually overestimated, while the planetary waves are usually underestimated, in agreement with previous studies performed on global weather forecasting models. When comparing the results of various versions of similar GCMs, it is clear that in some cases the vertical resolution of the atmosphere and, somewhat unexpectedly, of the adopted ocean model seem to be critical in determining the agreement with the reanalyses. The GCMs ensemble is biased with respect to the reanalyses but is comparable to the best 5 GCMs. This study suggests serious caveats with respect to the ability of most of the presently available GCMs in representing the statistics of the global scale atmospheric dynamics of the present climate and, a fortiori, in the perspective of modelling climate change.Comment: 39 pages, 8 figures, 2 table

Reconciling conflicting evidence for the cause of the observed early 21st century Eurasian cooling

It is now well established that the Arctic is warming at a faster rate than the global average. This warming, which has been accompanied by a dramatic decline in sea ice, has been linked to cooling over the Eurasian subcontinent over recent decades, most dramatically during the period 1998–2012. This is a counter-intuitive impact under global warming given that land regions should warm more than ocean (and the global average). Some studies have proposed a causal teleconnection from Arctic sea-ice retreat to Eurasian wintertime cooling; other studies argue that Eurasian cooling is mainly driven by internal variability. Overall, there is an impression of strong disagreement between those holding the “ice-driven” versus “internal variability” viewpoints. Here, we offer an alternative framing showing that the sea ice and internal variability views can be compatible. Key to this is viewing Eurasian cooling through the lens of dynamics (linked primarily to internal variability with some potential contribution from sea ice; cools Eurasia) and thermodynamics (linked to sea-ice retreat; warms Eurasia). This approach, combined with recognition that there is uncertainty in the hypothesized mechanisms themselves, allows both viewpoints (and others) to co-exist and contribute to our understanding of Eurasian cooling. A simple autoregressive model shows that Eurasian cooling of this magnitude is consistent with internal variability, with some periods exhibiting stronger cooling than others, either by chance or by forced changes. Rather than posit a “yes-or-no” causal relationship between sea ice and Eurasian cooling, a more constructive way forward is to consider whether the cooling trend was more likely given the observed sea-ice loss, as well as other sources of low-frequency variability. Taken in this way both sea ice and internal variability are factors that affect the likelihood of strong regional cooling in the presence of ongoing global warming.</p